the drought essay

Essay on Drought

Students are often asked to write an essay on Drought in their schools and colleges. And if you’re also looking for the same, we have created 100-word, 250-word, and 500-word essays on the topic.

Let’s take a look…

100 Words Essay on Drought

Understanding drought.

Drought is a natural event that happens when an area gets less rain than normal. It can last for months or even years.

Causes of Drought

Droughts often occur due to lack of rain. Sometimes, high temperatures can also cause drought by making water evaporate from soil and plants.

Effects of Drought

Drought can make it hard for plants and animals to survive. It can also lead to water shortages for people. In severe cases, drought can cause famine.

Dealing with Drought

People can deal with drought by conserving water, using it wisely, and planning for dry periods.

250 Words Essay on Drought

Introduction.

Drought is a natural disaster characterized by a prolonged period of abnormally low rainfall, leading to a shortage of water. It is a complex phenomenon that can have serious ecological, social, and economic impacts.

Droughts are primarily caused by irregularities in global weather patterns. Climate change has been identified as a significant factor, with increasing global temperatures leading to changes in rainfall patterns and increased evaporation rates. Human activities, such as deforestation and overuse of water resources, can also exacerbate drought conditions.

Impacts of Drought

Drought can have severe consequences for both the environment and human societies. It can lead to crop failure, livestock death, and water shortages, impacting food production and access to clean water. This can consequently lead to malnutrition, disease, and death, particularly in vulnerable populations. Economically, droughts can result in increased prices and job losses in agricultural sectors.

Drought Mitigation

Mitigation strategies for drought include water conservation, efficient irrigation techniques, and the development of drought-resistant crops. Additionally, improving climate forecasting can help societies prepare for and manage drought conditions. Policymakers must also prioritize sustainable water management to ensure that water resources are used efficiently and equitably.

Drought is a pressing global issue that requires concerted efforts to mitigate its impacts. By understanding its causes and consequences, we can develop effective strategies to manage drought and reduce its harmful effects on society and the environment.

500 Words Essay on Drought

Droughts occur when there is an extended period of below-average precipitation. This deficiency of water supply can last for months or even years. Droughts are categorized into three types: meteorological, agricultural, and hydrological. Meteorological droughts are associated with reduced rainfall, agricultural droughts with soil moisture deficits affecting crop production, and hydrological droughts with reduced water availability in streams, reservoirs, and aquifers.

The primary cause of drought is a lack of precipitation over an extended period. This can be due to natural climate variability, such as the El Niño Southern Oscillation, or changes in atmospheric conditions that suppress the formation of clouds and rainfall. Human activities, such as deforestation and overuse of water resources, can also contribute to the occurrence and severity of droughts.

Drought Management and Mitigation

Effective drought management requires a proactive approach, focusing on reducing vulnerability and enhancing resilience. Strategies can include improving water infrastructure, implementing water conservation practices, and developing drought-tolerant crops. At the policy level, it involves developing comprehensive drought management plans, early warning systems, and drought risk insurance. Climate change adaptation strategies also play a crucial role in drought mitigation.

Drought is a significant global challenge that requires concerted efforts to mitigate and adapt. While it is a natural phenomenon, human activities have exacerbated its occurrence and impacts. Therefore, understanding drought, its causes, impacts, and management strategies is essential for sustainable development and resilience. As we move forward, it is crucial that we continue to enhance our knowledge and strategies to better manage and mitigate the effects of droughts.

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The Problem of Drought on Earth Essay

• To find inspiration for your paper and overcome writer’s block
• As a source of information (ensure proper referencing)
• As a template for you assignment

The earth goes through different climates, normally based on temperature and precipitation differences. Most of the organisms found on the earth’s surface have developed mechanisms to adapt to different climates, though some climatic conditions are too harsh for these animals. Drought is one of the worse climatic changes since it does not only interfere with the water cycle, but every living thing found on the earth’s surface.

The worst thing that has happened in the current century is not depletion of energy sources, nor is it an increase in nuclear war but loss in the biodiversity. The other catastrophes can be repaired within a very short period but loss in biodiversity would take millions of years to correct.

The biggest threat to biodiversity is drought; this can either occur due to natural processes or can be influenced by human beings. Management and conservation measures of the South African reserve should be aimed at establishing ways of preventing the current biodiversity as well as investing in others.

When planning on the conservation measure to adapt for the South African reserve, certain issues have to be put into consideration; both biodiversity and the ecosystem must be preserved for future generation. Since the drought is affecting the vegetation for grazers, it is likely that most of them will die or be eaten by the predators (the lions and dogs).

This may not continue for long as all the grazers may be killed and some may die out of starvation leaving no food for the predators. This calls for urgent conservation measures in order to ensure that neither the grazers nor the predators become extinct.

Many organisms are able to thrive in the habitations that they are most adapted to, for example, fish cannot be able to survive outside water because they have special features that enable them to stay in water. The same applies to wildlife which cannot be able to thrive in an area without vegetation. Conservation measures should therefore be aimed at preserving the vegetation so as to provide a habitat for the wildlife

One way of conserving the reserve would be to transfer the lions and dogs and some of the grazers to other reserves with plenty of food in order to conserve the affected reserve and ensure that none of the organisms get extinct. Transferring the predators and some of the grazers would not be enough because even after doing that the carrying capacity of the reserve remains low and thus the remaining grazers will soon die of hunger.

Other conservation measures have to be adopted for instance planting of turf grass. Almost every cultural landscape contains turf grass lawn, which dictates the infrastructural aesthetic held by people and enforced by ordinance. The lawn is a landscape that requires regular watering yet does not get wet and require limited use of fertilizer and is always short.

The landscape is in essence designed to separate itself from the two most important components it needs, that is, water and resources. This is the heritage of a cultural endeavour to create a water-loving landscape that cannot put up with water.

Drought may be caused by increased human activities and thus the conservation plan must include measures on how to control such activities. It is true that human influences have led to the accelerating rate of climate change. In most cases, the human activities on land such as pollution and deforestation interfere with the water cycle. These activities do not only affect the aquatic life but also the natural cycle of water.

The aquifer table is depleted leading to increased surface runoff. If man was able to balance his activities with the water cycle, then there could be a strong relationship between land and water where each depend on the other one. Many people have changed their perspective about the environment and are now using measures of conserving it.

As we all know, drought is caused by lack of rainfall and the latter is being influenced by human activities such as deforestation and over-cultivation. To respond to this issue, trees should be planted and the government should issue bans to prevent the exploitation of the ecosystem. With all these measures being put into place, we expect the effects of the drought to decline although this may take quite some time.

Human beings in many parts of the world have become more conscious on the role played by living organisms. For instance, forests and vegetations are believed to regulate the amount of carbon dioxide in the atmosphere thereby controlling the rate of global warming.

Measures have been put in place to ensure that certain areas are left as reserves and most governments have gone to the extent of planting forests. This has created an increase in the habitat of most species and the rate of extinction which has increased significantly is expected to go down.

If the number of reserves is increased in South Africa, animals would be distributed evenly in these reserves and the impacts of the drought would not be as severe as if the number of reserves is limited.

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1. IvyPanda . "The Problem of Drought on Earth." May 7, 2019. https://ivypanda.com/essays/drought-essay/.

Bibliography

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What is drought? Causes, impact & countries most affected

East Africa is facing its worst drought in 40 years, with over 1.4 million people displaced by drought in Somalia alone. Learn more about drought, what causes it, and how we can support those most impacted.

Around the world, droughts are becoming increasingly common due to rising global temperatures — and have serious impacts, leading to crop failures, famine and malnutrition. 

East Africa , for example, is facing its worst drought in years, affecting 40 million people. Many are facing near-famine and malnutrition because of the drought’s impact on food supplies. 

Learn more about drought, what causes it, and what the IRC is doing to help in East Africa. 

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What is drought .

Drought is caused by a lack of rainfall, causing serious water shortages. It can be fatal.  

More specifically, drought is defined by a period of unusually dry weather caused by low rainfall and high temperatures. It is also defined in terms of the impact on agriculture when crops fail due to lack of moisture in soil, leading to food shortages and serious human impacts such as famine in severe cases. 

Unlike other extreme weather events that are more sudden, like earthquakes or hurricanes, droughts happen gradually. But they can be just as deadly as other weather hazards—if not more so. Drought has affected more people in the last 40 years than any other natural disaster.  

The severity of drought worsens over time. When it arrives, drought can last for weeks, months, or years—sometimes, the effects last decades. 

What causes drought?  

Droughts can be triggered by natural causes such as weather patterns. But increasingly they are caused by human activity. 

Human causes of drought 

Climate change : Global warming makes extreme weather more likely. It can make places drier by increasing evaporation. When land becomes so dry, an impermeable crust forms, so when it does rain, water runs off the surface, meaning sometimes flash flooding occurs. 

Deforestation : Plants and trees capture and release water into the atmosphere, which creates clouds and then rain. Scientists have observed a relationship between deforestation and drought. 

Agriculture : Intensive farming contributes to deforestation in the first instance but can also affect the absorbency of the soil, meaning it dries out much more quickly. 

High water demand : There are several reasons water demand might outweigh the supply, including intensive agriculture and population spikes. Also, high demand upstream in rivers (for dams or irrigation) can cause drought in lower, downstream areas. 

Other natural causes of drought 

Changes in ocean temperatures : El Niño and La Niña are climate patterns that can cause drought in some parts of the world. El Niño is characterized by warmer-than-average ocean temperatures in the Pacific Ocean, which can lead to drought in the southwestern United States and southern Africa. La Niña is characterized by cooler-than-average ocean temperatures in the Pacific Ocean, which can lead to drought in Australia and Indonesia. 

The jet stream : The jet stream is a band of strong winds that flows high in the atmosphere. Changes in the jet stream can cause drought in some areas by bringing in dry air from other parts of the world. 

How are people impacted by drought? 

Risk of famine .

Drought causes food insecurity when crops fail. When a substantial part of the population can no longer access food this is known as famine and results in widespread acute malnutrition, disease and death across the affected region. 

East Africa is currently experiencing widespread food shortages and near-famine, with millions of children under 5 suffering from severe acute malnutrition. 

Malnutrition 

A lack of nutritious food caused by food shortages leads to acute malnutrition. Children suffering from malnutrition are a high risk category. Deprived of essential vitamins and minerals required for their proper growth, they are prone to disease, severe developmental delays and even death.   

Effective treatment for children suffering from malnutrition exists, but often does not reach those most in need. The IRC has developed a simplified process for treating malnutrition in order to reach more children with lower costs. 

Increase in diseases 

Drought affects vital access to clean drinking water. This can lead to people drinking contaminated water, which brings about outbreaks of diseases like cholera and typhoid. These diseases can also spread in places with poor sanitation, another side-effect of having no clean water. 

It can cause wildfires 

Dry conditions can cause wildfires that burn remaining vegetation and endanger homes. Fires can also impact air quality and exacerbate chronic lung conditions. 

People are displaced 

People must travel further to find clean water. This usually falls to women and children, who must sacrifice other work and school to carry out an incredibly physical task. 

Without access to clean water or food, many must permanently leave their homes in order to survive. The World Health Organization states , “Water scarcity impacts 40% of the world’s population, and as many as 700 million people are at risk of being displaced as a result of drought by 2030.” 

Related : Meet the people displaced by drought in Somalia  

It can feed into conflict 

Research has also found that drought exacerbates existing conflicts. People migrating en masse from areas of drought and famine can result in increased political tensions and conflict due to increased competition for resources. There is evidence that drought contributed to the conflict in Syria , for example. 

Flash flooding 

Flooding can also be a risk in the same geographical areas that suffer from drought. 

Rain after a drought sounds like it ought to be a good thing, but after a prolonged period of dryness, sudden heavy rainfall can lead to hazardous flash flooding like that seen in Pakistan.  

This is because droughts leave the ground hard and baked, with little to no plant cover and low soil quality, which prevents rain from saturating the ground. Instead, when waterfalls in a large quantity and at speed—like in a thunderstorm—it runs over the parched ground. 

Which countries are in a drought? 

Droughts can occur all around the world. However, the effects of drought vary by region.  

Droughts bring the most risk to areas with high-pressure weather systems that are already prone to desertification. Developing countries are also more vulnerable to the socio-economic effects of drought due to a large percentage of their population being employed in the agriculture industry.  

East Africa 

In Africa droughts pose a high risk and the following countries in East Africa are severely affected by drought: 

Somalia where drought is leading to near-famine conditions 

Kenya which has experienced a record six below average rainy seasons 

Ethiopia has seen six below average rainy seasons in a drought affecting 31 million people 

Over 40 million people have been impacted by the drought across East Africa. The drought affecting countries like Somalia, Kenya and Ethiopia began in October 2020. Throughout these regions, insecurity, severe drought, and an exponential increase in food prices have brought millions to the brink of famine. 

“Somalia is seeing the worst of the crisis, with over 200,000 already living in the most extremes of hunger, but the challenge is regional,” says Abukar Mohamud, IRC’s Deputy Director of Programs for Somalia. “Across East Africa, people are facing the worst drought in 40 years.  

“People are not just dying due to a lack of food. Hunger means their weakened bodies cannot fight off diseases like diarrhea, measles or malaria, so death rates are high. Children are particularly at risk and often die at double the rate of adults. And those who survive will face ill health for the rest of their lives. The 2011 famine saw over 250,000 people die of hunger – half of whom were children.” 

What is the IRC doing to help in East Africa? 

East Africa is home to some of the IRC’s longest-running programs globally. Today, over 2,000 IRC staff in the region are scaling up our programs to address the current drought and rising food insecurity, including expanding to new areas to meet severe needs. 

This includes health programming, food and cash assistance, and providing clean water.  

A new approach to treating malnutrition 

Currently, 80% of malnourished children do not have access to treatment. The IRC has developed a streamlined approach for treatment so that more children can access treatment and recover. We are working to raise funds and remove blocks so that this treatment can be distributed at scale in places like East Africa.  

How can I help?

Around the world, our staff are working around the clock to ensure families can survive, recover and regain control of their futures. Donate now to support our work.

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Essay on Drought

Introduction

Imagine waking up to a day filled with sunshine, yet only a feeble trickle of water flows out as you turn on the faucet. This scenario, though fictional for many, mirrors the harsh reality millions face during droughts. Drought, a prolonged period of abnormally low precipitation, disrupts the rhythm of daily life, impacting everything from agriculture to industry to personal well-being. In this essay, we explore the intricacies of drought, including its origins, extensive repercussions, and the pressing requirement for viable solutions to alleviate its catastrophic impact on communities globally.

Types of Droughts

Drought manifests in various forms, each with distinct characteristics and impacts on different societal and environmental sectors. Here are the main types of drought:

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• Meteorological Drought: Meteorological drought manifests when a particular region experiences an extended period of precipitation significantly below its usual levels. A deficit in rainfall primarily characterizes it compared to the long-term average for that area. This type of drought can lead to dry soil conditions, reduced groundwater levels, and decreased surface water availability.
• Agricultural Drought: Agricultural drought occurs when the moisture content in the soil falls below the threshold necessary to sustain robust crop growth and development. It results in a lack of water for agricultural activities, potentially causing crop failure, reduced yields, and livestock loss. Agricultural drought can have severe economic repercussions, impacting food security, livelihoods, and rural economies.
• Hydrological Drought: Hydrological drought is associated with deficits in water supply within hydrological systems such as rivers, lakes, and reservoirs. It occurs when prolonged periods of low precipitation and reduced runoff diminish water availability in surface water bodies and groundwater aquifers. Hydrological drought can result in decreased water levels in rivers and reservoirs, reduced hydropower generation, and restrictions on water use for irrigation, industry, and domestic purposes.
• Socioeconomic Drought: Socioeconomic drought refers to the impacts of water scarcity on human populations and socioeconomic activities. It encompasses drought’s direct and indirect consequences on communities, economies, and societies. Socioeconomic drought can lead to food and water shortages, loss of income and employment, increased poverty and inequality, and social unrest. It highlights the interplay between environmental conditions, water management practices, and societal vulnerabilities in shaping the overall impact of drought events.

Causes of Drought

Drought is a complex phenomenon influenced by a combination of natural processes and human activities. Here are some of the main causes of drought:

• Climate Variability and Change: Variations in atmospheric circulation patterns, like the El Niño-Southern Oscillation (ENSO), can induce shifts in precipitation distribution, leading to intervals of diminished rainfall and subsequent drought conditions. Climate change exacerbates drought conditions by altering temperature and precipitation patterns, increasing the frequency, intensity, and duration of drought events in many regions.
• Deforestation and Land Degradation: Deforestation disrupts the water cycle by reducing transpiration and evaporation, decreasing rainfall, and increasing runoff. Land degradation, including soil erosion and desertification, reduces soil moisture retention and inhibits vegetation growth, exacerbating drought conditions.
• Overuse and Mismanagement of Water Resources: Overextraction of groundwater for irrigation, industry, and domestic use depletes aquifers, reducing groundwater recharge rates and exacerbating drought conditions. Inefficient water management practices, such as unsustainable irrigation methods and inadequate water storage infrastructure, can exacerbate water scarcity during drought.
• Urbanization and Population Growth: Urbanization alters land cover and increases impervious surfaces, reducing infiltration and groundwater recharge rates, exacerbating surface water runoff and flooding, and exacerbating drought conditions in nearby areas. Population growth increases water demand for domestic, industrial, and agricultural purposes, putting additional pressure on water resources and exacerbating drought conditions.
• Changes in Land Use and Agricultural Practices: Conversion of natural habitats to agriculture and urban areas alters the hydrological cycle, leading to changes in evapotranspiration, precipitation patterns, and runoff, exacerbating drought conditions. Intensive agricultural practices, such as monoculture farming and excessive irrigation, deplete soil moisture and degrade soil quality, increasing vulnerability to drought.
• Natural Variability and Extreme Weather Events: Natural climate variability, such as periodic fluctuations in ocean temperatures and atmospheric circulation patterns, can lead to prolonged periods of reduced rainfall and drought. Extreme weather events, such as heatwaves and prolonged dry spells, exacerbate drought conditions by increasing evaporation rates and reducing soil moisture.

Impacts of Drought

The impacts of drought are multifaceted and can affect various aspects of the environment, economy, society, and public health. Here’s a detailed explanation of the impacts of drought:

1. Agricultural Impacts

• Reduced Crop Yields: Drought leads to soil moisture deficits, hindering seed germination, crop growth, and development. As a result, farmers experience reduced crop yields and lower productivity.
• Livestock and Pasture Losses: Limited availability of water and forage resources during drought periods can lead to livestock deaths, decreased milk production, and loss of grazing land, impacting the livelihoods of farmers and pastoralists.
• Economic Losses: Agricultural drought results in significant economic losses for farmers, agribusinesses, and rural economies due to reduced crop yields, livestock losses, and increased production costs.

2. Water Supply Impacts

• Decreased Surface Water Availability: Drought reduces streamflow, river levels, and reservoir storage, decreasing water availability for municipal, industrial, and agricultural purposes.
• Groundwater Depletion: Prolonged periods of drought can deplete groundwater reserves as groundwater pumping increases to compensate for reduced surface water supplies, leading to long-term declines in aquifer levels.
• Water Quality Degradation: Decreased water flows and increased water temperatures during drought can exacerbate water quality issues, such as elevated concentrations of pollutants and contaminants, posing risks to human health and ecosystems.

3. Environmental Impacts

• Ecosystem Stress: Drought causes stress to terrestrial and aquatic ecosystems, leading to reduced vegetation cover, habitat degradation, and loss of biodiversity. Sensitive ecosystems such as wetlands, forests, and freshwater habitats are particularly vulnerable to drought-induced changes.
• Increased Wildfire Risk: Drought creates dry and combustible conditions, increasing the risk of wildfires. These wildfires can devastate forests, grasslands, and wildlife habitats, leading to habitat loss, soil erosion, and air quality degradation.
• Desertification and Land Degradation: Prolonged drought accelerates desertification and land degradation processes, leading to soil erosion, loss of arable land, and degradation of natural resources, exacerbating food insecurity and rural poverty.

4. Socioeconomic Impacts

• Food and Water Scarcity: Drought-induced crop failures and water shortages can lead to food and water scarcity, threatening food security and livelihoods, particularly in rural and marginalized communities.
• Economic Disruption: Drought disrupts economic activities, reduces agricultural output, and affects industries reliant on water resources, leading to job losses, decreased incomes, and reduced economic growth.
• Social Displacement: Drought-induced food and water scarcity, coupled with economic hardships, can trigger population displacement, migration, and conflicts over natural resources, exacerbating social tensions and inequalities.

5. Public Health Impacts

• Waterborne Diseases: Drought diminishes both the availability and quality of water, heightening the likelihood of waterborne illnesses like diarrhea, cholera, and typhoid fever due to inadequate sanitation and hygiene protocols.
• Malnutrition and Food Insecurity: Drought-related crop failures and food shortages can lead to malnutrition, especially among vulnerable populations such as pregnant women, children, and the elderly, exacerbating existing health disparities.
• Mental Health Issues: Drought-induced stress, anxiety , and depression can affect individuals and communities, particularly those facing financial hardships, social disruptions, and environmental losses.

Case Studies of Drought

Here are three case studies of significant drought events from different regions of the world:

1. California Drought (2012-2016)

• Duration: The California drought, often called the “worst drought in 1,200 years,” lasted from 2012 to 2016.
• Impacts: The drought had widespread impacts across California, affecting agriculture, water supply, ecosystems, and communities. Reduced snowpack in the Sierra Nevada Mountains led to decreased surface water availability, while groundwater levels declined due to increased pumping for irrigation. Agricultural losses amounted to billions of dollars, with farmers facing fallowed fields and crop failures. Urban areas implemented water restrictions, conservation measures, and drought emergency declarations to cope with dwindling water supplies.
• Response: California implemented various measures to address the impacts of the drought, including water conservation mandates, groundwater management reforms, investments in water recycling and desalination projects, and habitat restoration initiatives. The state also developed long-term water management strategies to enhance drought resilience and adapt to future climate challenges.

2. Australian Millennium Drought (1997-2009)

• Duration: The Australian Millennium Drought, one of the most severe droughts in Australia’s recorded history, lasted from 1997 to 2009.
• Impacts: The drought affected large parts of Australia, including the southeastern states of New South Wales, Victoria, and South Australia. Declining rainfall, depleted water reservoirs, and drying rivers led to severe water shortages for urban, agricultural, and environmental purposes. Crop yields declined, livestock numbers decreased, and ecosystems suffered from reduced water availability and habitat degradation. The drought also exacerbated water allocation and management conflicts between different sectors and regions.
• Response: Australia implemented various measures to mitigate the impacts of the drought and build resilience to future drought events. These measures included water restrictions, water efficiency programs, investment in water infrastructure and recycling projects, implementation of drought relief programs for farmers, and reforms in water governance and management practices. The Millennium Drought prompted significant policy reforms, such as the National Water Initiative, to improve water allocation, conservation, and management across the country.

3. Sahel Drought (1968-1974)

• Duration: The Sahel Drought, a prolonged period of drought and famine, occurred in the Sahel region of West Africa from 1968 to 1974.
• Impacts: The drought had devastating impacts on the Sahelian countries, including Senegal, Mauritania, Mali, Burkina Faso, Niger, Nigeria, Chad, Sudan, and Ethiopia. Declining rainfall, crop failures, and livestock losses led to food shortages, malnutrition, and famine, affecting millions of people. The drought exacerbated environmental degradation , desertification, and soil erosion, further reducing agricultural productivity and exacerbating poverty and social unrest in the region.
• Response: The Sahel Drought prompted international humanitarian assistance efforts, including food aid, emergency relief, and development assistance programs. National governments and international organizations implemented drought mitigation and adaptation measures, including drought-resistant crop varieties, water harvesting techniques, reforestation projects, and soil conservation practices. The drought also underscored the imperative for long-term strategies to tackle the underlying vulnerabilities in the Sahel region, including poverty , environmental degradation, and insufficient infrastructure.

Coping Strategies and Solutions

Coping with drought requires a combination of short-term measures to address immediate needs and long-term solutions to build resilience and adapt to changing climate conditions. Here are some coping strategies and solutions:

• Water Conservation and Efficiency Measures : Introduce water-saving technologies and methodologies across agricultural, industrial, and residential sectors, including drip irrigation, rainwater collection, and the use of efficient water fixtures. Promote public awareness and education campaigns on water conservation and efficient water use behaviors. Enforce water restrictions and regulations to limit non-essential water use during drought periods.
• Diversification of Water Sources : Allocate resources towards alternative water sources like recycled water, desalinated seawater, and treated wastewater to complement conventional water reserves during periods of drought. Develop decentralized water supply systems, including decentralized rainwater harvesting and decentralized wastewater treatment systems, to enhance water resilience at the local level.
• Drought-Resistant Agriculture : Promote the adoption of drought-resistant crop varieties and agroforestry practices that require less water and are more resilient to drought stress. Implement soil conservation measures, such as mulching and tillage, to improve soil moisture retention and reduce soil erosion during drought. Encourage sustainable land management strategies, such as crop rotation, cover crops, and integrated pest control, to improve soil fertility and boost drought resistance.
• Water Demand Management : Implement demand management strategies, such as water pricing mechanisms, water metering, and incentives for water conservation, to reduce overall water consumption and mitigate drought impacts. Encourage water-efficient land use planning and development practices, including green infrastructure and low-impact development, to minimize water demand and maximize water retention in urban areas.
• Ecosystem Restoration and Conservation : Restore and protect natural ecosystems, such as wetlands, forests, and riparian zones, that provide critical ecosystem services, including water regulation, flood control, and groundwater recharge. Implement watershed management strategies, such as reforestation, soil conservation, and habitat restoration, to enhance ecosystems’ resilience to drought and mitigate downstream impacts on water quality and quantity.
• Community-Based Adaptation : Foster community participation and collaboration in drought preparedness and response efforts, including community-based monitoring, early warning systems, and local water management initiatives. Build social capital and strengthen community resilience through capacity-building, livelihood diversification, and social safety nets to support vulnerable populations during droughts.
• Policy and Governance Reform : Develop and implement integrated water resource management policies and plans prioritizing sustainable water use, ecosystem protection, and climate resilience. Strengthen governance frameworks, institutional capacities, and regulatory mechanisms to ensure effective drought preparedness, response, and recovery at the local, national, and regional levels.

Policy and Government Initiatives

Policy and government initiatives are crucial in mitigating drought impacts and building resilience to water scarcity. Here are some examples of policies and initiatives implemented by countries around the world:

• Integrated Water Resource Management (IWRM) : Integrated Water Resources Management (IWRM) is a comprehensive water management approach incorporating the social, economic, and environmental aspects of water resources. Countries like South Africa have adopted IWRM principles in their national water policies to promote sustainable water use, equitable water allocation, and stakeholder participation.
• Drought Management Plans : Many countries have developed drought management plans to enhance preparedness, response, and recovery efforts during drought events. Australia’s National Drought Policy provides a framework for coordinated federal, state, and local drought management, including risk assessment, early warning, and emergency relief measures.
• Water Pricing and Market Mechanisms : Water pricing mechanisms, such as volumetric pricing and water markets, can incentivize efficient water use and allocation. Nations like Chile have adopted water markets, enabling users to purchase, sell, and exchange water rights, fostering water conservation, and enhancing allocation efficiency.
• Water Rights and Allocation Reforms : Reforming water rights systems and allocation mechanisms can improve water use efficiency, equity, and sustainability. Mexico’s National Water Law introduced water rights reforms, establishing a system of water permits and concessions to regulate water use and promote environmental conservation.
• Climate Change Adaptation Strategies : Nations are incorporating climate change adaptation strategies into their water management policies to tackle the effects of climate variability and change, including drought occurrences. The European Union’s Water Framework Directive incorporates climate change considerations into water management planning and implementation to enhance water resilience and ecosystem protection.
• Investments in Water Infrastructure : Enhancing water infrastructure investments, including the construction of dams, reservoirs, and water treatment plants, can bolster both the reliability of the water supply and its resilience to drought. China’s South-to-North Water Transfer Project is one of the largest water infrastructure projects in the world. It aims to transfer water from water-rich regions in the south to water-stressed regions in the north to alleviate water scarcity and drought risks.
• International Cooperation and Agreements : International cooperation and agreements are essential for addressing transboundary water issues and sharing best practices in drought management. The Nile Basin Initiative brings together countries in the Nile River basin to promote cooperation, sustainable development, and joint management of shared water resources, including measures to address drought and climate risks.

Future Challenges and Opportunities

As we look ahead, several challenges and opportunities emerge in the context of drought management and resilience-building efforts:

• Climate Change Impacts : We expect climate change to worsen drought conditions globally, requiring proactive measures to reduce emissions and adapt to changing climate patterns.
• Water Scarcity and Competition : Population growth and increased water demand intensify competition for limited water resources, requiring sustainable water management practices and equitable allocation mechanisms.
• Ecosystem Vulnerability : Droughts threaten ecosystems substantially, resulting in habitat degradation and biodiversity loss. Therefore, conservation and restoration initiatives are vital for bolstering ecosystem resilience.
• Socio-Economic Vulnerability : Vulnerable communities bear the brunt of drought impacts, facing food insecurity and poverty. Addressing social vulnerabilities and promoting inclusive development are essential for resilience.
• Technological Innovation : Technological advancements like remote sensing and data analytics present opportunities for enhanced drought monitoring and early warning systems, thereby augmenting preparedness and response capabilities.
• Policy and Governance Reform : Strengthening policy frameworks and governance mechanisms is crucial for effective drought management. Integrated approaches and multi-stakeholder collaboration are needed to foster resilience.
• Community Resilience and Empowerment : Empowering local communities and building social capital are key to enhancing drought resilience. Investing in community-led initiatives and capacity-building programs can promote sustainable development.

Drought remains a significant threat, exacerbated by climate change and increasing water demands. However, proactive measures such as water conservation, community resilience-building, and policy reform offer hope for mitigating its impacts. Embracing technological advancements, fostering multi-stakeholder collaboration, and prioritizing community empowerment are vital for navigating future challenges. Investing in sustainable water management practices and adaptive strategies can build resilience and ensure a more resilient future in the face of drought. Together, we can address the complexities of drought and create a more sustainable and equitable world for generations to come.

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Drought: Everything You Need to Know

Drought affects more people globally than any other natural disaster. Here’s what causes these prolonged dry spells and how we can mitigate their impact.

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Natural disasters usually announce their arrival: Hurricanes uproot trees, tornadoes roar, and wildfires wipe out entire landscapes. These large, sudden events generate destruction on impact—and then they’re gone.

Drought is different. It doesn’t make a big entrance—the start of a drought might even be mistaken for a bit of a dry spell—and its impact builds over time. But while often described as a “ creeping disaster ,” drought leaves a trail of destruction as dangerous and deadly as any other extreme weather event. In fact, drought has affected more people around the world in the past four decades than any other type of natural disaster.

Here’s a look at what drought is, what causes it, and how we can better prepare for its impact.

What is drought?

Types of drought, causes of drought, are droughts increasing, drought prevention and preparation.

Drought is characterized by a lack of precipitation —such as rain, snow, or sleet—for a protracted period of time, resulting in a water shortage. While droughts occur naturally, human activity, such as water use and management, can exacerbate dry conditions. What is considered a drought varies from region to region and is based largely on an area’s specific weather patterns. Whereas the threshold for drought may be achieved after just six rainless days on the tropical island of Bali, annual rainfall would need to fall below seven inches in the Libyan desert to warrant a similar declaration.

Developing nations are particularly vulnerable to the impacts of climate change, including drought. More than 80 percent of drought-induced economic damage and loss suffered by developing nations from 2005 to 2015 was related to livestock, crops, and fisheries. The economic toll of some $29 billion tells only part of the story. Drought in developing nations is notorious for creating water and food insecurity and exacerbating preexisting problems such as famine and civil unrest. It can also contribute to mass migration, resulting in the displacement of entire populations.

A refugee camp in Kenya

IHH Humanitarian Relief Foundation/Flickr

In the United States, drought is the second-most costly form of natural disaster (behind hurricanes), exacting an average toll of $9.6 billion in damage and loss per event, according to the National Oceanic and Atmospheric Administration's (NOAA) National Centers for Environmental Information. Meanwhile, some level of drought often has some part of the country in its grip. During the historic dry spell of 2012 (the nation’s most extensive since the 1930s ), as much as two-thirds of the country was affected by drought at its peak. U.S. droughts can be persistent as well. From 2012 to 2016, scant rainfall and record-breaking heat in California created what is estimated to have been the state’s worst drought in 1,200 years .

These dry spells take a major toll on the economy, with the drought and extreme heat of 2012 alone resulting in an estimated $17 billion in crop loss es. As in developing nations, they can create conditions of water insecurity and higher food prices. Drought can also lead to regionally specific problems. In California, for example, a large number of native fish populations that depend on the San Francisco Bay–Delta Estuary —from the bellwether delta smelt to the iconic Chinook salmon—have suffered sharp declines due to reduced river flows during the recent historic drought.

Droughts are categorized according to how they develop and what types of impact they have.

Drought damage on the Fresno Harlen Ranch in Fresno, California

Cynthia Mendoza/USDA

Meteorological drought

Imagine a large swath of parched, cracked earth and you’re likely picturing the impact of meteorological drought, which occurs when a region’s rainfall falls far short of expectations.

Agricultural drought

When available water supplies are unable to meet the needs of crops or livestock at a particular time, agricultural drought may ensue. It may stem from meteorological drought, reduced access to water supplies, or simply poor timing—for example, when snowmelt occurs before runoff is most needed to hydrate crops.

Hydrological drought

A hydrological drought occurs when a lack of rainfall persists long enough to deplete surface water—rivers, reservoirs, or streams—and groundwater supplies.

Natural Causes

Droughts have plagued humankind throughout much of our history, and until recently they were often natural phenomena triggered by cyclical weather patterns, such as the amount of moisture and heat in the air, land, and sea.

Fluctuating ocean and land temperatures

Ocean temperatures largely dictate global weather patterns, including dry and wet conditions on land, and even tiny temperature fluctuations can have huge ripple effects on climate systems. Research shows that dramatic and prolonged temperature changes in the North Pacific and North Atlantic Oceans correspond directly to extreme weather patterns on land, including persistent droughts in North America and the eastern Mediterranean—the latter of which has been described as the region’s worst drought in 900 years . Fluctuating ocean temperatures are also behind El Niño and La Niña weather phenomena, with La Niña notorious for drying out the southern United States . Meanwhile, hotter surface temperatures on land lead to greater evaporation of moisture from the ground, which can increase the impact of drought.

Altered weather patterns

The distribution of rainfall around the world is also impacted by how air circulates through the atmosphere. When there is an anomaly in surface temperatures—particularly over the sea—air circulation patterns are altered, changing how and where precipitation falls around the world. The new weather patterns can throw water supply and demand out of sync, as is the case when earlier-than-usual snowmelt reduces the amount of water available for crops in the summer.

Reduced soil moisture

Soil moisture can impact cloud formation, and hence precipitation. When water from wet soil evaporates, it contributes to the formation of rain clouds, which return the water back to the earth. When land is drier than usual, moisture still evaporates into the atmosphere, but not at a volume adequate to form rain clouds. The land effectively bakes, removing additional moisture and further exacerbating dry conditions.

Manmade Causes

While drought occurs naturally, human activity—from water use to greenhouse gas emissions—is having a growing impact on their likelihood and intensity.

Climate change

Climate change—and global warming , specifically—impacts drought in two basic ways: Rising temperatures generally make wet regions wetter and dry regions drier. For wetter regions, warm air absorbs more water, leading to larger rain events. But in more arid regions, warmer temperatures mean water evaporates more quickly. In addition, climate change alters large-scale atmospheric circulation patterns, which can shift storm tracks off their typical paths. This, in turn, can magnify weather extremes, which is one reason why climate models predict the already parched U.S. Southwest and the Mediterranean will continue to get drier.

Excess water demand

Drought often reflects an imbalance in water supply and demand. Regional population booms and intensive agricultural water use can put a strain on water resources, even tipping the scale enough to make the threat of drought a reality. One study estimates that from 1960 to 2010, the human consumption of water increased the frequency of drought in North America by 25 percent. What’s more, once rainfall dwindles and drought conditions take hold, persistent water demand—in the form of increased pumping from groundwater, rivers, and reservoirs—can deplete valuable water resources that may take years to replenish and permanently impact future water availability. Meanwhile, demand for water supplied by upstream lakes and rivers, particularly in the form of irrigation and hydroelectric dams, can lead to the diminishing or drying out of downstream water sources, which may contribute to drought in other regions.

Drought-stricken Lake Powell, seen from space

Deforestation and soil degradation

When trees and plants release moisture into the atmosphere, clouds form and return the moisture to the ground as rain. When forests and vegetation disappear, less water is available to feed the water cycle, making entire regions more vulnerable to drought. Meanwhile, deforestation and other poor land-use practices, such as intensive farming, can diminish soil quality and reduce the land’s ability to absorb and retain water. As a result, soil dries out faster (which can induce agricultural drought), and less groundwater is replenished (which can contribute to hydrological drought). Indeed, experts believe the 1930s Dust Bowl was caused in large part by poor agricultural practices combined with the cooling of the Pacific and the warming of the Atlantic by as little as a few tenths of a degree.

The Intergovernmental Panel on Climate Change (IPCC) did not see a global trend toward increasing dryness or drought across the world in 2013, when it released its most recent assessment. But global temperatures have unequivocally become hotter, and hotter conditions precipitate extreme weather —including severe drought. Hotter conditions also reduce snowpack, which provides a key source of water supply and natural water storage in many regions. Regionally, the driest parts of the earth are getting drier, while the wettest parts are getting wetter. That’s why some areas of the world, such as southern Europe and West Africa, have endured longer and more intense droughts since the 1950s while other regions, such as central North America, have seen droughts become less frequent or less intense. Looking forward, as temperatures continue to rise, the IPCC and other researchers anticipate an intensification of those regional trends.

Cattle farm near Walkaway, western Australia

Jackocage/Flickr

We can’t control the weather. But by limiting our climate change contributions, reducing water waste, and using water more efficiently, we can prepare for—and maybe even curb—future dry spells.

Climate change mitigation

The impact of climate change, including more severe drought, can be mitigated only when countries, cities, businesses, and individuals shift away from the use of climate-warming fossil fuels to cleaner renewable energy sources . The Paris Agreement, which was adopted by nearly every nation in 2015 and aims to limit the earth’s warming over the next century to 2 degrees Celsius, or 1.5 degrees if possible, lays the framework for global climate action. But the current commitments countries made under the pact so far aren’t considered enough to limit global warming to 2 degrees Celsius. It will succeed only if countries go beyond their commitments, and that includes the United States. However, catering to big polluters instead of the will of a majority of Americans, the Trump administration had committed to withdrawing the country from the agreement, as well as from key domestic policies—from the Clean Power Plan to automotive fuel efficiency standards —that would reduce our nation’s carbon emissions. Fortunately, American states and cities , as well as more than 2,000 U.S. businesses, institutions, and universities, are taking the reins on climate action by reducing emissions and increasing energy efficiency. It’s crucial that they do, as research indicates even meeting the agreement’s most ambitious targets will only reduce—not eliminate—the likelihood of extreme weather events.

There’s plenty of room for individuals—particularly Americans, who produce about four times more carbon pollution than citizens elsewhere, on average—to fight climate change as well. Actions include speaking to local and congressional leaders about regional environmental policies and finding ways to cut carbon pollution from your daily life.

Urban water conservation and efficiency

The U.S. Environmental Protection Agency (EPA) estimates that aging infrastructure—faulty meters, crumbling pipes, leaky water mains—costs the United States an estimated 2.1 trillion gallons in lost drinkable water each year. (That’s about enough to drown Manhattan in 300 feet of water.) Meanwhile, a single leaky faucet—releasing just three drips a minute—wastes more than 100 gallons of water in a year. States, cities, water utilities, businesses, and citizens can curb water waste by investing in climate-smart strategies . These include repairing leaky infrastructure (from utility pipes to the kitchen faucet), boosting water efficiency with the use of water- and energy-efficient technologies and appliances (such as clothes washers ), and adopting landscape design that makes use of drought-tolerant plants and water-efficient irrigation techniques. In California, these strategies alone could reduce water use by as much as 60 percent . For individuals, there are many other ways to conserve water as well.

Water recycling

Recycled water —also called reclaimed water—is highly treated wastewater that can be used for myriad purposes, from landscape irrigation (such as watering public parks and golf courses) to industrial processes (such as providing cooling water for power plants and oil refineries) to replenishing groundwater supplies. Graywater—recycled water derived from sinks, shower drains, and washing machines—can be used on site (for example, in homes and businesses) for non-potable uses such as garden or lawn irrigation. Recycled water can serve as a significant water resource, reducing demand from sources such as rivers, streams, reservoirs, and underground water supplies. According to California’s Department of Water Resources, recycling has the potential to increase water supply in the state by as much as 750 billion gallons a year by 2030.

Stormwater capture

Every year in the United States, about 10 trillion gallons of untreated stormwater washes off paved surfaces and rooftops, through sewer systems, and into waterways. Not only does this create pollution problems (as contaminants from land get flushed into rivers, lakes, and oceans), but it reduces the amount of rainwater that soaks back into the earth to replenish groundwater supplies. The use of green infrastructure —including green roofs, tree plantings, rain gardens, rain barrels, cisterns, and permeable pavement—can increase water supplies substantially. Stormwater capture in urban Southern California and the San Francisco Bay region alone could potentially increase annual water supplies by as much as 205 billion gallons .

Farms affected by drought near Strasburg, Colorado

Lance Cheung/USDA

Agricultural water conservation and efficiency

Agriculture is the largest consumer of the earth’s available freshwater, accounting for 70 percent of withdrawals globally, according to the World Bank. Strategies for better water management in the agricultural sector focus on increased water efficiency and reduced consumption. These include improved irrigation techniques—such as switching from flood to drip irrigation, which alone can cut water use by about 20 percent—as well as more precise irrigation scheduling to adjust the amount of water used at different stages of crop growth. Meanwhile, crop rotation, no-till farming (a method for growing crops with minimal soil disturbance), and the use of cover crops help build soil health, which in turn enables the land to absorb and retain more water. Indeed, the use of cover crops alone on just half the land used to grow corn and soybeans in 10 of America’s highest-producing agricultural states would help the soil retain as much as a trillion gallons of water each year.

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ENCYCLOPEDIC ENTRY

Below-average precipitation affects the amount of moisture in soil as well as the amount of water in streams, rivers, lakes, and groundwater.

Earth Science, Climatology, Conservation, Anthropology

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A drought is a period of time when an area or region experiences below-normal precipitation . The lack of adequate precipitation , either rain or snow, can cause reduced soil moisture or groundwater , diminished stream flow, crop damage, and a general water shortage. Droughts are the second-most costly weather events after hurricanes.

Unlike with sudden weather events such as hurricanes, tornadoes, and thunderstorms, it is often difficult to pinpoint when a drought has started or when it has ended. The initial effects of a drought may be difficult to identify right away, so it may take weeks or months to determine that a drought has started. The end of a drought is hard to identify for the same reason. A drought may last for weeks, months, or even years. Sometimes, drought conditions can exist for a decade or more in a region. The longer a drought lasts, the greater the harmful effects it has on people.

Droughts affect people in a several ways. Access to clean drinking water is essential for all life, and sources of water may dwindle during a drought . Without the presence of water, people must bring in enough water from elsewhere to survive. Water is also needed for crops to grow. When not enough precipitation falls to naturally water crops , they must be watered by irrigation . Irrigation is possible only when there is enough water in nearby rivers, lakes, or streams, or from groundwater . During a drought , these water sources are diminished and may even dry up, preventing crops from being irrigated and causing them to die off.

One person studying these problems is Alexandra Cousteau, a National Geographic Emerging Explorer whose latest initiative is Blue Legacy. She started Blue Legacy to raise awareness that we live on a water planet and must take care of it. Cousteau, the granddaughter of the famed ocean explorer Jacques Cousteau, believes that water will be a crucial issue in this century. She predicts that water problems such as drought , storms, floods, and degraded water quality will create “water refugees :” people migrating in search of water. Cousteau stresses that we must do all we can to protect Earth’s valuable freshwater resources.

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Essay on Drought | Drought Essay for Students and Children in English

February 13, 2024 by sastry

Essay on Drought: India is situated in the Northern Hemisphere extending from 8° 4′ N to 37° 17′ N latitude. The Tropic of Cancer passes through the middle of the country, thus the country falls into tropical as well as sub-tropical zones. The country gets two complete showers of seasonal rain, one during summer season called South-West monsoon and one in winters called the North-East monsoons.

The rest of the year is practically dry. The rain bearing winds are called monsoon winds which persistently flow in the same direction and get reversed only with the change of seasons.

You can read more  Essay Writing  about articles, events, people, sports, technology many more.

Long and Short Essays on Drought for Kids and Students in English

Given below are two essays in English for students and children about the topic of ‘Drought’ in both long and short form. The first essay is a long essay on Drought of 400-500 words. This long essay about Drought is suitable for students of class 7, 8, 9 and 10, and also for competitive exam aspirants. The second essay is a short essay on Drought of 150-200 words. These are suitable for students and children in class 6 and below.

Long Essay on Drought 500 Words in English

Below we have given a long essay on Drought of 500 words is helpful for classes 7, 8, 9 and 10 and Competitive Exam Aspirants. This long essay on the topic is suitable for students of class 7 to class 10, and also for competitive exam aspirants.

The agriculture in India is largely dependent upon the monsoon rain shower during the months of June to the middle of September and a few parts of the country gets rains during the retreating monsoon from October to December. Tamil Nadu, South of Andhra Pradesh, South-East of Karnataka and Kerala get the maximum showers during the time, about 75 cm.

The occurrence and quality of monsoons depends upon the intensity of winds blowing over the Arabian Sea, the Indian Ocean and the Bay of Bengal. Sometimes, the country receives intense rainfall and there are times when the monsoon gets weak and there are scanty rains here and there.

Moreover, there is the problem of unequal distribution of rainfall over the country where the monsoon is extremely active whereas the same monsoon is barely active in other parts of the country. In other words, by the time it reaches the higher regions, the winds have shed most of their moisture already or they weaken so much that nothing is left in them in terms of momentum and so they shed their moisture on the way.

This uncertain and uncontrolled character of monsoons in India causes the problem of droughts at some places. Droughts occur when rainfall during a particular year fails to reach even the average or normal level expected of the place at that time of the year. Droughts usually occur in places which have a high variability between low and heavy amount of rainfall.

The greater the difference, more are the chances of droughts. Thus droughts in India occur mainly when South-West monsoon is weak and ineffective. A weak monsoon results in scanty or no rainfall; hence leading to droughts. Many a times droughts occur due to untimely arrival of monsoon-either it is too late or too early. In either case, agriculture is most severely affected. Prolonged breaks between consecutive spells of rain, too, aggravates the problem.

In India, on an average, a drought affects about 16% of the total agricultural land and about 50 million population. The areas that are regularly affected by droughts are those which receive an annual rainfall below 75 cm or have a high variability of 40 cm or more. There are about 99 districts which receive annual rains below 75 cm. A total of 68% of sown area is subject to drought in varying degrees.

But surprisingly the severest droughts have occurred in comparatively humid and wet areas such as West Bengal, Bihar and Odisha. These regions usually get high rainfall but a slight failure of rainfall can cause severe droughts here simply because of high intensity of population and the near total dependence of agriculture on monsoon rains in these regions. A normal drought affects a huge part of the country’s population, hence making the drought into a severe one.

This leads to a vicious circle of misery, especially for that part of the population, which is practically hand to mouth. Even among these, the landless labourers are the ones who suffer the most because they are the first ones to lose their jobs due to failure of rains.

Less people are thus required to till the land and so they are the first ones to be pushed over the crevices of hunger, poverty, starvation and destitution. Lack of irrigation facilities and total dependence on monsoon rains leads to even more severe droughts in the remote parts of the country. Moreover, due to the ecological imbalance, the frequency of droughts is likely to increase.

The failure of rains in 2014, has led to the possibility of it being declared as a ‘drought year’. Till August, 2014, 36% of the nation’s meteorological regions faced moderate to severe drought. Punjab, Haryana and Uttar Pradesh, India’s ‘grain’ bearer belt, is reeling under severe drought. As a result, farmers are paying sky-high prices to protect their paddy crop.

Hopefully, due to great technological advances, irrigation facilities and developments in the transport system, with even the remotest villages getting connected to nearby towns and cities, the intensity with which the droughts can affect human population, agriculture and cattle can be reduced to some extent. The governments now prefers to keep surplus stocks of food grains as well as fodder to combat such recurrent crisis with the support of voluntary organisations, NGOs etc.

NASA scientists, including one scientist of Indian origin have developed a new satellite to predict the severity of droughts and help farmers maximise crop yield. At present, there is no ground or satellite-based global network for monitoring soil moisture at a local scale. It would be of great help to developing countries like India, if this technology gets introduced soon.

Short Essay on Drought 200 Words in English

Below we have given a short essay on Drought is for Classes 1, 2, 3, 4, 5 and 6. This short essay on the topic is suitable for students of class 6 and below.

The Government of India through Crisis Management Framework 2011, aims at identification of fundamental aspects of drought prone areas, phases of crisis, magnitude, outcome of crisis to trigger mechanism and strategic response matrix. The Central Research Institute for Dryland Agriculture (CRIDA), under ICAR has been assigned the task to prepare district-wise contingency plans in collaboration with State Agricultural Universities, Indian Council of Agricultural Research (ICAR) institutes and Krishi Vigyan Kendras (KVKs).

The programme also works toward long-term goals such as maintenance of ecological balance by developing, conserving and even harvesting all kinds of resources including land, water, livestock and human resources. It also aims at minimising the adverse effects of droughts on crops and livestock through use of appropriate technology and the naturally available resources.

The recent initiatives by Government were special assistance package and higher seed subsidy. It is also planning to extend subsidy on diesel to areas where there has been less than 50% rainfall. In case, drought is declared by any state, the government has proposed a ₹ 700 crore scheme for cultivation of horticultural crops and ₹ 100 crore for fodder production. Agricultural crop insurance scheme is also in the pipeline. It’s high time that India implements robust drought mitigation measures. The entire burden or blame shouldn’t be put on the farmers. They must be protected and fully prepared for natural calamities. Their prosperity is nation’s progress.

Drought Essay Word Meanings for Simple Understanding

• Persistent – constantly repeated, continued
• Scanty – barely sufficient
• Momentum – force or speed of movement, impetus, as of a physical object or course of events
• Variability – apt or liable to vary or change; changeable
• Consecutive – following one another in uninterrupted succession or order, successive
• Vicious circle – a sequence of reciprocal cause and effect in which two or more elements
• Intensify and aggravate each other, leading to a worsening of the situation
• Crevices – a crack forming an opening
• Destitution – lack of the means of subsistence, utter poverty
• Matrix – the cultural, social, or political environment in which something develops
• Subsidy – a grant or contribution of money
• Mitigation – the act of making a condition or consequence less severe
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Drought Essay in English for Students

August 12, 2021 by Sandeep

Essay on Drought: It is a closely associated natural disaster caused due to scanty or no rainfall. They are life-risking and take a heavy toll on poultry, human, and wildlife. An extreme water shortage causes crops to dry, and farmers run helter-skelter for their livelihood. Soil loses its retention capacity, and huge plots of fertile land turn into barren fields where nothing can be cultivated. Global warming and greenhouse gases mainly cause the drought situation to occur.

Essay on Drought

Below we have provided Drought Essay in English, suitable for classes 6, 7, 8, 9 & 10. This detailed essay on drought of 200-250 words is greatly helpful for all school students to perform well in essay writing competitions.

Drought is a natural calamity where there is a water shortage everywhere, even for essential needs. People in many countries are suffering from drought, and others are losing their lives because of the lack of water that contributes to food shortages. The effect of drought is terrible, and the affected country often has trouble returning to a healthy state. In some areas, starvation, as a result of drought, leads to several people’s death. Drought also affects crops’ production, causes forest fires, and leads to insufficient electricity production.

Causes of Drought

The principal explanation for drought is the lack of rain. If the usually falling rain fails for a couple of months, then water shortage occurs. Wells get dry, and people and other living beings begin travelling in search of water from one location to another. Though the leading cause of drought is lack of rainfall, other factors also contribute to such a situation.

Trees are the principal source of rainfall. When we cut the trees to build houses, we kill vegetation and greenery and eliminate the Earth’s primary source of rain. The rivers, lakes, and ponds are the natural ways water is collected on Earth. Activities such as excessive irrigation and improper water use for agricultural purposes remove the surface water from these natural reservoirs and create a drought condition.

India is a land that is dependent on monsoon rainfall for water adequacy. Consequently, insufficient rain in most parts of the world is considered the primary cause of the drought. High sea temperatures have resulted in the El Nino impact that has further influenced the monsoon season’s onset. Together with unsuitable agricultural practices and increased pollution levels, all these factors have contributed to a decline in monsoon rainfall that has led to a drought.

Consequences of Drought

Biodiversity disruption and depletion occur during a drought when many species die from lack of water and food. Drought severely affects the health of both animals and plants. Drought effects cause dehydration and malnutrition, which weaken humans and plants alike. Extreme malnutrition of humans and animals leads to their death.

The economic losses suffered during drought are also significant. Drought causes plants to die and deteriorate, reducing economic, agricultural production. Food production costs will increase, and water economic activities such as tourism and energy production will be reduced. India’s agriculture sector is the most vulnerable to climate conditions. Much of India’s agriculture relies on both rainfall and groundwater.

“Drought” like situation has tremendously affected India’s farming sector and animal husbandry. The scorching sun sucks the groundwater and becomes fatal to the cattle. Continuous drought can cause the soil to lose its humidity and fertility. There is no rain in many areas, so we can see that the lands would have cracks on them. After several years of rain, some areas recover their fertile soil, but some entirely lose their ability to produce crops.

Residents queue to fill water bottles at a natural water spring in Cape Town, South Africa, a city that may soon have to shut off its taps due to a severe water shortage.

From Not Enough to Too Much, the World’s Water Crisis Explained

Many more cities than Cape Town face an uncertain future over water. But there are emerging solutions.

“Day Zero,” when at least a million homes in the city of Cape Town, South Africa, will no longer have any running water , was originally scheduled for April. It was recently moved to July . The three-year long drought hasn’t ended, but severe water rationing—limiting people to a mere 13 gallons (50 litres) per person per day—has made a difference. (To put this into perspective, an average U.S. citizen uses 100 gallons (375 liters) per day .)

“No person in Cape Town should be flushing potable water down a toilet any more.… No one should be showering more than twice a week now,” said Helen Zille , the premier of the Western Cape province, where Cape Town is located.

Like many places in the world, Cape Town and the surrounding region has likely reached “peak water,” or the limit of how much water can be reasonably taken from the area, says water scientist Peter Gleick , president-emeritus of the Pacific Institute. Gleick, who has spent substantial time in South Africa, says the country generally has good water managers.

“Two years ago, I would not have predicted Cape Town would face day Zero,” he said in an interview. However, climate change has disrupted the Earth’s hydrological cycle (water cycle), changing when, where, and how much precipitation falls. That has made water management planning far more challenging, he said. Yet our water systems were largely built based on the more stable climate of the past.

“What’s happening in Cape Town could happen anywhere,” says Gleick.

Global Risk

Brazil’s São Paulo, a megacity of 20 million, faced its own Day Zero in 2015. The city turned off its water supply for 12 hours a day, forcing many businesses and industries to shut down . In 2008, Barcelona, Spain, had to import tankers full of freshwater from France. Droughts have also become more frequent, more severe, and affecting more people around the world.

Fourteen of the world’s 20 megacities are now experiencing water scarcity or drought conditions. As many as four billion people already live in regions that experience severe water stress for at least one month of the year, according to a 2016 study in the journal Science Advances . Nearly half of those people live in India and China. With populations rising, these stresses will only mount.

Disaster data compiled by the U.N . clearly shows floods are also getting worse. They are happening more frequently, especially in coastal regions and river valleys, and affecting more people. Of all major disasters in the world between 1995 and 2015, 90 percent were weather-related events, such as floods, storms, heatwaves, and droughts. Flooding accounted for more than half of all weather-related disasters, affecting 2.3 billion people and killing 157,000 in that 20-year period. Last year, the costs of extreme weather—floods, droughts, wildfires, storms—in the U.S. reached a record-topping $300 billion . These events displaced more than one million Americans from their homes.

Humanity is facing a growing challenge of too much water in some places and not enough water in others. This is being driven not just by climate change, but by population and economic growth and poor water management, experts warn.

“Water scarcity and flood problems are primarily due to quick growth, increasing vulnerability, and insufficient preparation,” says Arjen Hoekstra , a professor of water management at the University of Twente in the Netherlands. “Climate change, however, is and will worsen the situation in most cases.”

The Roll of “Embedded Water”

Cape Town, where nearly four million people live, has a dry climate much like southern California. It is facing it’s Day Zero due to increased water demands from population and economic growth in combination with a three-year drought that’s severely limited the water supply. Yet what many people don’t realize is that typical home use of water—for washing, flushing, and cooking—represents only about three percent of humanity’s total water consumption, says Hoekstra. Agriculture uses the lion’s share, 80 to 90 percent, followed by energy production and industry.

Rivers Run Dry

The Cape Town region is the heart of South Africa’s wine country, which exported 113 million gallons (428.5 million litres) of wine in 2016 to Europe and the U.S. Yet this export represents a much bigger amount of water that was used to grow and process the grapes. Most of that water is no longer available for human consumption, according to Hoekstra, who is the creator of the water footprint concept. He and colleagues at the Water Footprint Network have worked out that it takes between 26 to 53 gallons (100 to 200 liters) of water to grow the grapes and process them into one five-ounce (125 ml) glass of wine.

In other words, the net amount of water used to grow or make something, be it a lemon, cellphone, or glass of wine, is the product’s water footprint. Most of the water used to make a typical glass of wine is lost to evaporation, with a small amount stored in the grapes, and the rest unsuitable for reuse. While the evaporated water will eventually become rain, it is unlikely to fall over the same vineyards, or even in the Western Cape province, meaning it is effectively “lost” to the region.

So that means a typical 25-ounce (750 ml) bottle of wine has a water footprint of nearly 200 gallons (750 liters). That means the region’s 2016 wine exports involved the net consumption of 113.2 billion gallons (428.5 billion liters) of water. This is water that is lost to the region.

South Africa already has 7 million people without access to water . Meeting their needs would require 33.3 billion gallons (126 billion liters) per year, one third of the amount the wine industry consumes. On top of that, the Western Cape exported an estimated 231,000 tonnes of citrus fruits , mostly oranges, in 2017. The water footprint of one orange—the net amount of water used to grow it—averages 21 gallons (80 liters). Using that basis, those citrus exports used up 30 billion gallons (115 billion liters) of the province’s water.

Not only does it take water to grow anything, it also takes water to make most things: cars, furniture, books, electronics, buildings, jewelry, toys, and even electricity. This water, which often goes largely unseen, is often called “virtual water.” What gets forgotten is that virtual water is as real as the water you drink.

South Africa, a water-stressed country, also exports oil products, minerals, and metals, all of which require enormous amounts of water. For example, it exported 211 tonnes of platinum in 2012. That’s like an export of 45 billion gallons (170 billion liters) of water—the estimated amount of water needed to mine and process the metal .

Other large countries with growing populations, such as China and India, also export staggering volumes of virtual water, often while facing considerable water scarcity problems at home. “This simply can’t continue,” says Hoekstra.

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Seeking solutions.

All of those exports could be produced using far less water, Hoekstra says. It starts with what he calls the most important water management strategy: grow and produce things in the right place. In other words, water-intensive crops like rice and cotton should be grown in water-rich regions.

In a global economy, drought can be a big issue even in water-rich countries, because of a growing dependence on imports. Around 38 percent of the European Union’s water consumption is reliant on water availability in other countries, to grow soybeans, rice, cotton, and other products that it imports. “That makes Europe vulnerable to increasing water scarcity and drought,” says Christopher Briggs , executive director of Water Footprint Network.

A coastal city, Cape Town hopes to solve its problem by getting a new water source: the ocean. It is building its first desalination plants . However, these are expensive and energy intensive. Gleick says it would be more cost effective for the region to shift to less-water intensive crops and to reuse treated wastewater. Currently, Cape Town reuses just five percent of its treated wastewater, compared to Israel’s 85 percent. Israel has also eliminated water-thirsty crops like cotton and made major improvements in water efficiency to free up more water for population growth.

California, which recently suffered through four years of drought and water restrictions , also needs to shift its agricultural production to less water-using crops, says Gleick, who is based there. And the state could increase its wastewater reuse from the current 15 percent, using the surplus to recharge depleted aquifers and use on crops.

A reservoir can be seen at a low level in Cape Town in February. Many other cities could suffer similar fates in the near future, experts warn.

When There’s Too Much Water

Perhaps ironically, too much water too fast was California’s most recent water problem. Following its worst wildfire season in history, heavy rainfall this winter produced mud slides that killed more than 20 people and destroyed or damaged hundreds of homes. Hurricane Harvey , which hit Texas and Louisiana last August, causing $125 billion in damage, dumped more water out of the sky than any storm in U.S. history. Some 890,000 families sought federal disaster aid, most often from flooding in the Houston area—in large part because many homes were built on flood plains . At the start of March, five states were under a state of emergency (Louisiana, Kentucky, Indiana, Missouri, and Michigan) due to heavy rainfalls and flooding.

Rapid population growth, building on floodplains or low-lying coastal regions, and climate change are the biggest reasons why flooding is affecting more people and causing ever greater damage, warns Gleick.

Climate change is the result of burning fossil fuels and has added 46 percent more heat-trapping carbon dioxide to the atmosphere. But even if fossil-fuel used ended today, that additional heat in the atmosphere will put 10 times more Americans at risk of being flooded out by rivers over the next 20 years, a new study reveals .

“More than half of the United States must at least double their protection level within the next two decades if they want to avoid a dramatic increase in river flood risks,” says lead-author Sven Willner from Germany’s Potsdam Institute for Climate Impact Research (PIK).

Rainfall changes caused by global warming will increase river flood risks across the globe, the study found. In South America, the number of people affected by river flooding will likely increase from 6 to 12 million. In Africa, the number will rise from 25 to 34 million, and in Asia from 70 to 156 million.

It bears repeating that these findings are based on the current level of carbon dioxide in the atmosphere. In reality, humanity added 45 billion tons in 2017, and will likely add that much or more in 2018. Without limiting human-caused warming to well below 3.6 degrees F (2 degrees Celsius), the river flood risk in many regions will be beyond what we can adapt to, Willner and team’s study concludes.

Climate change is also causing sea levels to rise, resulting in substantial coastal flooding during high tides and storms. More than 13 million Americans living on the coasts will be forced to move by 2100 because of rising ocean levels, according to a 2017 study by Mathew Hauer, a demographer at the University of Georgia. About 2.5 million will flee the region that includes Miami, Fort Lauderdale, and West Palm Beach. Greater New Orleans loses up to 500,000 people; the New York City area loses 50,000, the study estimated. These coastal migrants will likely go to cities on high ground with mild climates, such as Atlanta, Austin, Madison, and Memphis. ( See what would happen if all the ice melted .)

“If people are forced to move because their houses become inundated, the migration could affect many landlocked communities as well,” said Hauer in a statement.

Related Topics

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Essay on Drought

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Drought is a disaster which affects many regions of India every year. A natural disaster which leads to a shortage of water for drinking, agriculture and other practices is called a drought. However, we are yet to come up with some concrete measure in order to avoid this adverse situation through which the people have to go through each year.

Audience: The below given essays are exclusively written for school students (Class 5, 6, 7, 8, 9, 10, 11 and 12 Standard) and college students.

Drought is a severe condition in which some regions face a heavy shortage of water. There are some countries which are nowadays struggling with an insufficient amount of water. This situation occurs due to factors like climate change, deforestation or global warming.

In some areas, starvation as a result of drought, leads to the death of several people. Drought also affect the production of crops, causes forest fires and leads to insufficient electricity production.

It is important to adopt some solutions to tackle this issue. We can use methods like rainwater harvesting, seawater desalination or grow more plants and trees. The whole world is familiar with the misuse of water resources which needs to be overcome in order to prevent droughts.

The prolonged absence of rain or the lack of natural sources of water can bring about a drought. This natural phenomenon has been occurring all through the history of mankind and it has shaped many civilizations in the past. Droughts are something that people fear and it is also something that can be brought about by our actions towards our surrounding. One is compelled by practical reason to consider what actions can bring about potentially cataclysmic events like droughts and since I am still a student there is a lot I can do, further on as I go through life, to contribute to reasonable water usage.

The earth has its own principle of functioning and it changes our surrounding often and without warning, that’s why droughts sometimes happen even though we do nothing, in particular, to make them come about. When such events occur, people use different techniques to find alternative sources of water. The best we can do in such situations is to find tools that we can use to help us predict what the movement of water will be, or how much rain will fall.

On the other hand, we tend to misuse our natural resources and to drain them. That is why the recent decades have seen many rivers dry out due to our extensive agricultural needs. The lack of water brought about droughts in many regions that were previously famed for their natural wealth. Thankfully, people are becoming aware of how they are behaving and through this awareness, we are developing new methods for water use and distribution, it is up to us to implement those changes and make fear of the great drought a thing of the past.

“Drought” which results from the shortage of water due to lack of rainfall. The situation is challenging and can prove to be catastrophic for those living in the drought-affected areas.

Causes of Drought:

The Marathwada region of Maharashtra suffers from “drought” condition every year. There are various factors responsible for causing a “drought” like situation.

Some of these are discussed below:

1. Deforestation:

The main cause of “drought” is deforestation, which leads to a shortage of rainfall. Trees and shrubs hold the ground water, prevent it from evaporation and attracts rainfall. Deforestation is carried out to clear the land for farming, industrialization and urbanization. The soil in these areas loses its capacity to hold water, which also leads to “drought” condition. The devastating flood in the beautiful state of Kerala has become one of the biggest catastrophe in recent times.

2. Diminishing Water Bodies:

The usage of water bodies like rivers and lakes is done on a huge scale. During scorching summers these rivers and lakes are dried which result in dreadful “droughts”. Due to extreme climatic condition and various human activities, the water in these water bodies dries down which leads to “drought”. Wells are also a main sources of water in various regions in the country. Villages and towns in the states of Maharashtra and Gujarat are facing life threatening situation where water in the wells has dried up. People in these villages stand in long queues to purchase water for drinking and daily needs.

Effects of Drought:

The farming sector in India is the most vulnerable to the climatic condition. Most of the agriculture in India is dependent on rainfall and ground water. “Drought” like situation has tremendously affected the farming sector and animal husbandry in India. The scorching sun sucks the ground water and becomes fatal to the cattle.

Measures to Prevent Drought:

Droughts can be prevented by –

i. Planting more trees.

ii. Implementing water conservation techniques.

iii. Reducing wastage of water and water pollution.

Conclusion:

Although initiatives like the “Paani Foundation” are being taken to mitigate “drought” condition in India but not much is done till date. As a responsible citizen we must contribute to the efforts taken to combat “drought” condition so that our future generations will not face such crisis.

The problem of drought is very severe and there are plenty of different provinces in India which are being largely impacted. It is really important for people at large to understand that the time calls for taking some strict measures at the earliest.

We have exploited mother earth in a ruthless manner and owing to the anthropogenic exploitation; the natural balance of the ecosystem has been disturbed. This in turn has led to plenty of troubles which include drought.

Drought – Getting Familiar:

Drought mainly refers to the condition wherein the area receives almost negligible to nil rainfall making it a dry period. This can be really deadly for the farmers as most of the harvest won’t ripen and it has several adverse consequences. Granted there are artificial methods of irrigation and the option of water supply but not all farmers have access to these facilities. This infers that drought ends up wrecking havoc on their finances and the families of the farmers sometimes even end up committing suicide or dying because of starvation.

Remedial Measures:

This brings us to the question as to what can be done to remedy the situation of drought. The answerer lies in helping the environment. The environment has the power to heal itself, but we need to be supportive in our approach. It is extremely important to understand the grave concerns and the bleak future that awaits us.

Drought isn’t the only calamity which we are facing. The increased frequency of earthquakes, flash floods, depleting ice cover, striking change in climates are all symbolic of the piteous condition of our environment. Until and unless, we manage to educate the masses and enlighten them about the need to have a green cover and preserve the environment, the frequency of drought and other calamities will continue to be on the rise. More and more measures need to be taken and the ruthless exploitation of the environment needs to stop right away.

We know that it is easier said than done but the change needs to start from somewhere. You should make it a point to understand the possible areas wherein you can bring a change. Try by curtailing the cutting down of trees even if it is for development purpose. Use measures to combat pollution and stop the use of non bio-degradable products. It is the collective efforts which will end up making a huge difference.

Drought is a natural calamity which is an impending sign of the dark future which this planet might be enveloped in if we do not take the right action now!

What is a drought? As per the given definitions, it is a natural disaster resulting in scarcity of water for drinking, agriculture and industrial purposes. But, given the current scenario, is it actually a natural disaster. This may not be completely true as human activities over a period of time have resulted in altering of nature’s natural phenomenon and today we see droughts occurring at places which were once abundant with water resources. Hence there is a strong need to understand the causes of drought and what can be done to prevent or minimize it.

Drought Prone Regions in India:

Some states of India have been declared as drought-prone due to the frequent occurrence of drought year after year in these states. These states are Rajasthan, Andhra Pradesh, Orissa, Maharashtra and Northern Karnataka. Apart from these many regions, Gujarat, Uttar Pradesh and parts of other states are also affected by drought every year.

India is a land which is dependent on monsoon rainfall for adequacy of water. Hence inadequate rainfall is considered as the major reason for drought in most parts of the country. However, this is again a subject of debate as to why there has been insufficient rainfall for quite some years now. Another reason is the drip in the water table and consequently less water vapour in the atmosphere which is responsible for the formation of clouds.

Again global warming has led to changes in the normal climatic conditions and with the increase in temperatures; there has been a significant effect on the monsoon season in India as well. Moreover, high sea temperatures have led to the El Nino effect taking place which has further affected the onset of monsoon season. All these factors combined with improper agricultural practices and increase in pollution levels have contributed to the reduction in the monsoon rainfall which has led to drought each year in many areas in India.

What should be done?

There is an urgent need to have measures in place in order to save the regions of India from drought. One of the major plans of the Government in this regard is the linking of rivers. If we are able to link the rivers we can divert excess rivers from region to the drought-affected areas and save them from this disaster. Another important measure is to have proper irrigation methods in place so as to utilize water only as much as it is required. Moreover, extracting of water through tube wells and other sources should be checked into as this leads to drip in the water table which triggers the onset of drought.

Last, but not least, it is not the responsibility of the government alone to have measures in place to prevent regions from being affected by drought, we all should ensure that we save water to the maximum and follow the rules as laid down by the Government. We should do rainwater harvesting as well so that we store the water provided to us by nature which shall be helpful in difficult times. A collective effort by all can surely be helpful in minimizing if not preventing the situation as adverse as drought.

Introduction:

Drought is a miserable condition caused due to lack of water in a particular region or country or territory for a long period of time. Drought is a natural calamity in which there is scarcity of water everywhere even for the basic needs. People in many countries suffer due to drought and many lose their lives since lack of water leads to lack of food. The impact of drought is very horrible and sometimes it becomes difficult for the affected country to recover to a normal state.

The main reason for drought to occur is the absence of rain. When the normally falling rain fails for a few months then there arises water scarcity. Wells become dry and people and other living beings start to move from one place to another in search of water.

Although lack of rainfall is the main cause for drought , there are also other causes that lead to such a condition.

The various causes of drought are:

Now-a-days people are mis-treating the environment. Why there is no rain? What causes rain? Everyone should ask these questions to themselves to know the real cause of drought. Trees are the main source of rainfall. When we cut trees for constructing buildings, we are not only removing the vegetation and greenery but also removing the main source of rainfall from the Earth.

2. Draining of Surface Water:

Rivers, lakes, ponds are the natural ways by which water is stored in the Earth. Activities like excessive irrigation, excessive use of water for industrial purposes drains the surface water from these natural reservoirs and cause a condition known as drought. Rise in temperature due to global warming is also a cause for draining of water.

Impacts of Drought:

The impact caused by drought is so huge that many countries that faces drought year on year still remains as under-developed countries. The day-to-day activities of the people get stopped. The severity of drought can even take many lives. Let us look into some of the major impacts:

1. Heavy Loss to Farmers:

Agriculture is the source of living for the farmers. Periodic rainfall and the availability of ground water is very much important for agriculture. Drought impacts farmers the most because if there is no rainfall, agriculture fails. There is no yield, plants die, livestock suffers and farmers end up with no income. They get debts to try other ways and make their living but when everything goes out of control, they have no other way than to end their lives. Severe droughts lead to increase in the number of farmer suicides.

2. Loss of Wildlife:

It is during the time of drought, forest fires start occurring. Since everything is dry, fire catches up very easily. The life of wild animals is at huge risk; some get burnt in the forest fires and some lose their habitat and have to move to some other place.

3. Soil Degradation:

Continuous drought will make the soil lose its moisture and fertility. We can see at many places where there are no rains, the lands will have cracks on them. Some areas regain their fertile soil after many years of rain but some totally lose their nature to yield crops.

4. Safety is at Risk:

The scarcity of food leads to increase in prices of commodities. As the droughts might have taken the employment of some, no income would push people to commit crimes such as theft.

There are some ways that people can try to manage drought. Few important ones are listed below: –

People can use rain water harvesting method to save and store rain water and use it at emergency times like drought.

Waste water must be collected, purified and re-used. The water thus stored can be used for watering plants and can be used for irrigation also.

Afforestation techniques can be adopted.

Drought has huge consequences but it is not the end. If everyone of us contribute their share in preserving the environment, then many hazards like drought can be managed very easily.

Drought is a natural disaster that occurs in some regions of the globe. Some regions are more prone to drought while other regions are not. In India, drought has been experienced and a lot of people have died. Drought causes death of humans, animals and plants due to the adverse conditions that are harsh to the ecosystem and limits survival. In disaster management, drought is considered among the threats to human and animal life. Drought is defined as a prolonged period of inadequate water and food. The periods of drought vary but lack of water for over two weeks is considered drought.

During drought, the ecosystem is negatively affected that is why agriculture is compromised and it results in lack of food. The effects of drought are both to the animate and inanimate objects in the environment. Drought is handled by disaster management teams by provision of water and food to the affected people and prevention of further effects like fires on dry vegetation. Drought can occur naturally due to dry seasons or can result from human activities that causes a change in climate.

Lack of rainfall for long periods of time results in drought. Rain formation or precipitation processes require moisture accumulation in the atmosphere or on the ground as ice. Sunshine and winds can affect the precipitation processes as it affects the formation of water.

Another cue of drought is the natural dry seasons whereby low humidity is experienced. During the dry season, water sources dry up due to high temperatures that increase vaporization. In the high demand for vapor, extreme measures like drawing water from plants is reached which results in death of those plants.

Human activities could also result in drought. Agriculture and human settlements result in deforestation. Deforestations predispose the environment to erosion of soil and vegetation destruction. The lack of vegetation and forests causes decreased rainfall in the region and could cause drought occurrence.

Climatic changes also result in drought. Human activities like emission of greenhouse gases to the environment has caused global warming. In global warming, climate change is experienced such that the temperatures on the surface of the earth are raised. Raised temperatures result in increased vaporization and depletion of water from rivers, boreholes. Effects of global warming have been determined to be either extremes of rainfall or drought.

Consequences of Drought:

Drought causes adverse effect on the ecosystem. Interruption and loss of biodiversity is experienced during drought because animals of several species die due to lack of water and food. Also, the living things like trees and vegetation die. Diseases also arise during seasons of drought that affect living things and cause death. Extinction of rare species is common during seasons of drought.

The losses experienced in the economy during drought are substantial. Drought causes death and deterioration of plants thus decreasing the agricultural economical activities. There will be inflation of food production costs and diminished water economic activities like tourism and energy production.

Health of both animals and plants is greatly affected by drought. Drought effects cause diseases like dehydration and malnutrition that are debilitating to both humans and plants. Extreme hunger for humans and animals cause death.

Drought Management:

Once drought has occurred, the protection of people and animals should be done. In disaster management, the focus is on mitigating the consequences and providing life sustenance to those affected by the disaster. In agriculture, methods of irrigation and crop rotation have been implemented in arid areas so as to mitigate the consequences of drought. Water harvesting is also essential in preparation for drought. In water harvesting, construction of dams and boreholes in arid areas has been helpful during seasons of drought.

Erosion is minimized through crop rotation. Water conservation methods like recycling and outdoor use restrictions have been employed in arid areas.

In conclusion, drought is a natural disaster whose effects are adverse and cause loss of life. The management of drought generally involves the water conservation, storage and expansion of sources of water. The consequences of drought are deleterious and destruct the ecosystem and loss of biodiversity.

In order to reduce the consequences of drought, several measures have been put in place. Disaster management teams have conducted projects for water conservation for use during drought like by constructing dams. Mitigating the consequences of drought also involved the inhibition of causes of drought. Mitigation of erosion through planting enough vegetation to prevent erosion goes a long way in preventing drought. Human activities should also be controlled.

Drought can simply be defined as a form of natural disaster that is a result of the precipitation in a particular region below average which results in prolonged periods of water supply shortage, be it ground water, surface water or rainfall water. Droughts can go on for a lot of months or even years; it is most times declared and claimed after about just 15 days.

The agriculture and ecosystem of a particular region can be substantially impacted by drought and this can lead to a great deal of harm on the economy of the region. It has been discovered that the probability of a drought taking place and bush fires occurring is increased significantly by the dry seasons annually. Drought conditions are significantly worsened by long heat periods and this is as a result of the hastened evaporation of vapours of water.

There are a lot of species of plants like the Cactaceae family that have adaptations for the tolerance of drought (like a reduce area of leaf and cuticles that are waxy to help improve their drought tolerance ability). There are other species of plants that survive periods of droughts as seeds that are buried.

Grasslands and Deserts are examples of arid biomes that are produced by droughts that are semi-permanent. Humanitarian crisis and mass migrations are caused by prolonged droughts. Majority of ecosystems that are arid have very low productivity. The world experienced its longest period of drought in Atacama Desert of Chile and the drought lasted for about 400 years.

There are a lot of causes of drought.

A few out of the many causes will be discussed below:

1. Climate Changes:

Droughts are triggered by all the various activities that result in climate change globally and this can have a very strong effect on agriculture all over the world most especially in countries that are developing. Global warming and climate change will bring about an imbalance in the ecosystem.

There is going to be erosion and flooding in some regions and drought in other regions. Therefore, it is quite obvious that climate change and global are one of the leading causes of drought in the world today.

2. Deficiency in Precipitation:

Precipitation is produced through mechanisms including orographic rainfall, strati-form rainfall and convective rainfall. The processes of convective rainfall involve vertical motions that are strong and can lead to the atmosphere overturning in that particular location in about an hour, causing heavy precipitation. The processes of stratiform precipitation involve upward motions that are weaker, a little bit less intense and can last a duration that is longer.

We can divide precipitation into about three categories; this is based on if it falls in form of liquid water, water in liquid form that freezes when it comes in contact with a surface and ice. Droughts mainly occur in areas that the normal rainfall levels are quite low. If the factors in the region do not help the volume of precipitation in a way that they can get to the surface in time, drought occurs. Drought can also be triggered through a very high reflected sunlight level.

3. Dry Season:

In the tropic regions, we have distinct dry and wet seasons and this is as a result of the Monsoon trough. The occurrence of drought is greatly increased during dry seasons, this season is known by the very low humidity and rivers and watering holes drying up. As a result of the inadequacy of watering holes and rivers, a lot of animals that graze migrate because of the absence of water and move to areas that are more fertile. Some of the animals that do this include wildebeest, elephants, zebra and cattle.

As a result of the absence of water, bushfires are very common during this season. Because of the increased temperature, the water vapour tend to become more energetic, to increase the relative humidity to 100%, required water vapour is more. When it is warm, the rate of vegetable and fruit production is increased and this causes an increase in transpiration and evaporation from plants leading to drought conditions that are worse.

Types of Drought :

With the persistence of drought, all of the various conditions that surround it worsen gradually and the effect on the region increases gradually.

There are three major types of droughts:

i. Meteorological drought is a type of drought that occurs anytime we have a prolonged period of below average rainfall or precipitation. It is common for meteorological drought to precede other types of drought.

ii. Agricultural drought is a type of drought that affects the ecology and production of crops in a particular region. Agricultural drought can also happen independently as a result of a change in the levels of precipitation when erosion and soil conditions that are triggered by agricultural endeavours that are poorly planned lead to a drop in the amount of water that is available for crop use. However, traditional droughts are caused by a period of precipitation that is below average.

iii. Hydrological drought is a type of drought that occurs when the available water reserves in sources like reservoirs, lakes and aquifers drop below average. Hydrological drought takes a lot of time to manifest since it deals with water that has been stored and is used and not replenished.

The effects of water shortages can be grouped into three namely:

i. Social effects

ii. Economic effects

iii. Environmental effects

Droughts can also cause wars, wildfires, social unrest, and drop in electricity production, mass migration, hunger, famine and so many more.

Prevention Measures:

Prevention measures include:

i. Building of Dams

ii. Cloud seeding

iii. Desalination

iv. Proper Drought monitoring

v. Proper Land use

vi. Rainwater harvesting

vii. Restriction of water use outdoors

viii. Use of Recycled water

Drought can be very detrimental to the ecosystem and can also have a lot of effects. It is therefore extremely necessary that we do our possible best to battle drought and try to employ methods of drought relief, mitigation methods to prevent drought.

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Home — Essay Samples — Environment — Disasters — Drought

Essays on Drought

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Research Report on Drought in Australia

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Essay on Drought for Children and Students

Table of Contents

Drought is a condition when there are no rains for a long period of time. The occurrence of drought is a common sight in many parts of the country. The consequences of this condition are drastic and many times irreversible. Drought is the condition when certain parts of the world are deprived of rain for months or at times the entire season. There are several reasons that cause drought-like situations in different parts and prove to be fatal.

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Long and Short Essay on Drought in English

Here are some short and long essays on Drought of varying lengths to help you with the topic. You can choose any drought essay given below:

Drought Essay – 1 (200 words)

Drought which is marked by the absence of or low rain in a particular region for a long period of time occurs because of various reasons including global warming, deforestation and many other human activities. This climatic condition can cause disastrous impact on the environment as well as the living beings. Some of the effects of drought include failure of crops, financial loss, price rise and soil degradation.

Several Indian states have been hit by drought leading to mass destruction of crops and disruption of the normal functioning of the society. Many parts have even witnessed famine leading to the death of several people due to starvation. Looking at the adversities faced by people in such areas, the government of India has come up with various drought relief plans however a lot more needs to be done to control this problem and deal with its after effects.

Some of the solutions suggested in this direction are rainwater harvesting, recycling and reuse of water, controlling deforestation, sea water desalination, cloud seeding, growing more plants and trees, stopping overall waste of water. However, most of these cannot be achieved if the general public does not support the cause. Each one should thus take it as a responsibility to contribute his/ her bit to curb the problem.

Drought Essay – 2 (300 words)

Drought, which results in the shortage of water, is mainly caused due to lack of rainfall. The situation is problematic and can prove to be fatal for those living in the drought-affected areas. It is particularly a curse for the farmers as it destroys their crops. Continuous drought-like situation also leads to the soil becoming less fertile.

Causes of Drought

There are various factors that lead to drought. Here is a look at these causes in detail:

• Deforestation

Deforestation is said to be one of the main causes of shortage of rainfall that leads to drought. Adequate amount of trees and vegetation is required on land to limit evaporation of water, store enough water on land and attract rainfall. Deforestation and construction of concrete buildings in their place has caused a major misbalance in the environment. It lowers the capacity of the soil to hold water and increases evaporation. Both these are a cause of low rainfall.

• Low Surface Water Flow

Rivers and lakes are the main sources of surface water in various regions around the world. In extreme summers or because of usage of surface water for various human activities, the water in these sources dries down leading to drought.

• Global Warming

The negative impact of global warming on the environment is known to all. Among other issues, the emission of greenhouse gases that results in the rise in earth’s temperature has resulted in the rise in evaporation. High temperature is also a cause of wildfires that worsens the drought-condition.

Apart from these, excessive irrigation is also one of the causes of drought as it drains the surface water.

Though the causes of drought are largely known and are mostly the result of misuse of water resources and other non-environmental friendly human activities, nothing much is being done to curb this problem. It is time the governments of various countries should join hands to overcome this global issue.

Drought Essay – 3 (400 words)

Drought occurs when a region receives no or less than the average amount of rainfall leading to water shortage, failure of crops and disruption of normal activities. Various factors such as global warming, deforestation and construction of buildings have given rise to drought.

Types of Droughts

While some areas are marked by complete absence of rain for a long period of time, others receive less than the average amount of precipitation, yet others might face drought for some part of the year – So the severity and type of drought varies from place to place and from time to time. Here is a look at the different types of droughts:

• Meteorological Drought

When there is a reduction in rainfall in a region for a particular period – it can be for few days, months, seasons or year – it is said to be hit by meteorological drought. In India an area is said to be hit by meteorological drought when the annual rainfall is 75% less than the average rainfall.

• Hydrological Drought

This is basically associated with the reduction in water. Hydrological droughts are often a result of two successive meteorological droughts. These are divided into two categories:

• Surface Water Drought
• Ground Water Drought
• Soil Moisture Drought

As the name suggests, this situation involves inadequate soil moisture that hinders crop growth. This is an outcome of meteorological drought as it leads to lower water supply to soil and greater water loss due to evaporation.

• Agricultural Drought

When the meteorological or hydrological droughts lead to negative impacts on the crop yield in a region, it is said to be hit by agricultural drought.

This is said to be the most severe drought situation. People in such regions do not get any access to food and there is mass starvation and devastation. The government needs to intervene in such a situation and food is supplied to these places from other places.

• Socio-Economic Drought

This situation occurs when there is a decrease in the availability of food and loss of income due to the failure of crop and the social security and access to food for the people in such areas is at risk.

Drought is a difficult situation to deal with especially if the severity is high. Several people are affected due to drought each year. While the occurrence of drought is a natural phenomenon, we can certainly reduce the human activities that lead to such a situation. Government must also come up with effective measures to deal with its after effects.

Drought Essay – 4 (500 words)

Drought, a condition that occurs due to no or very low rainfall, has been classified into different categories including meteorological drought, famine, socio-economic drought, hydrological drought and agricultural drought. Whatever be the type of drought, it disturbs the normal functioning of the regions affected.

Impacts of Drought

The regions hit by drought take a good amount of time to recover from the disaster caused, particularly if the severity of the drought is high. Drought disrupts the day-to-day lives of the people and has a widespread impact on various sectors. Here is how this natural disaster impacts the lives of the people living in the affected region:

• Agricultural Loss

A major impact occurs on the agriculture and other related sectors as these are directly dependent on the ground and surface water. Loss of crop yields, low rate of livestock production, rise in plant disease and wind erosion are some of the major impacts of drought.

• Financial Loss for Farmers

Farmers are worst effected by drought. The crops in the drought hit areas do not yield and the farmers whose sole income is generated through farming are worst affected by this situation. In an attempt to make their ends meet, many farmers end up in debt. The cases of farmer suicides due to such situation are also common.

• Wildlife at Risk

The cases of forest fires increase during droughts and this puts the wildlife population at high risk. Forests get burnt down and many wild animals end up losing life while others lose their shelter.

The prices of various cereals, fruits, vegetables rise because of low supply and high demand. The prices of food items such as jams, sauces and drinks that are produced from those particular fruits and vegetables also increase. In certain cases, goods are imported from other places to meet the demands of the people and hence the prices levied on the same are high. The retailers who offer goods and services to the farmers also face financial loss due to reduced business.

• Degradation of Soil

The soil loses moisture due to continuous drought and its quality degrades. It takes a lot of time for some areas to regain the ability to yield crops.

• Overall Impact on Environment

Damage is caused to various species of plants and animals, there is degradation of landscape quality and biodiversity is impacted. The quality of air and water is also affected due to drought. While some of these conditions are temporary others may last long and might even turn permanent.

• Public Safety at Stake

Lack of food and increased prices of different commodities may give rise to crimes such as theft and this can put public safety at stake. Conflict may also occur between water users thereby causing tension among general public.

Drought Prone Countries

Some of the countries that are more prone to drought include Albania, Afghanistan, Armenia, Bahrain, Northeast parts of Brazil, Burma, Cuba, Morocco, Iran, China, Bangladesh, Botswana, Sudan, Uganda, Somalia, Eritrea and Ethiopia.

Drought is one of the most disastrous natural calamities. Famine, that is the most severe forms of drought, ends in major socio, economic and environmental loss for the regions affected.

Drought Essay – 5 (600 words)

Drought, a condition when certain regions are faced with scarcity of water due to low or no rainfall, has been the cause of several problems in India. There are many areas in the country that are hit by drought each year while others are faced with this condition occasionally. Drought is caused due to various factors such as deforestation, global warming and inadequate surface water and has severe impact on the lives of the people living in the affected areas as well as the general health of the environment.

Drought Prone Areas in India

Many regions in the country are hit by drought each year. Statistics reveal that approximately one-sixth of the total geographical area of the country that inhabits around 12% of the population is drought prone.

One of the most drought prone states in the country is Rajasthan. As many as eleven districts in this state are hit by drought. These regions receive scanty or no rainfall and have low level of ground water. Drought is also a common phenomenon in the state of Andhra Pradesh. Almost every district here is hit by drought each year.

Here is a look at some of the other regions in the country that face frequent drought:

• Saurashtra and Kutch, Gujarat
• Coimbatore in Kerala
• Mirzapur Plateau and Palamu, Uttar Pradesh
• Kalahandi, Orissa
• Purulia, West Bengal
• Tirunelveli District, South of Vaigai River, Tamil Nadu

Possible Solutions for Drought

• Rain Water Harvesting

This is the technique of collecting and storing rainwater in tanks and natural reservoirs to use it later. Rain water harvesting must be made mandatory for all. The idea behind this is to put the available water to use.

• Sea Water Desalination

Sea water desalination must be done so that the vast amount of water stored in the sea can be used for the purpose of irrigation and other agricultural activities. The government must make major investment in this direction.

• Recycle Water

Waste water must be purified and recycled for reuse. This can be done in many ways. Small steps such as installing rain barrel, collecting the waste water from RO systems, usage of shower buckets, saving water from washing veggies and creating rain garden can help in this direction. The water collected by these means can be used to water the plants.

• Cloud Seeding

Cloud seeding is done to modify weather. It is a way to increase the amount of precipitation. Potassium iodide, silver iodide and dry ice are some of the chemicals used for the purpose of cloud seeding. The government should invest in cloud seeding to avoid drought in the areas prone to this condition.

• Plant More Trees

Deforestation and the building of concrete structures is one of the causes of scanty rainfall. Efforts must be made to plant more trees. This simple step can change the climatic conditions and also bring about other positive changes in the environment.

• Water Usage

Each one should take it as a responsibility to stop the wastage of water so that there is availability of enough water even when during times of low rainfall. Government must take steps to keep a check on the usage of water.

• Campaigns must be Run

The government must run campaigns stating the benefits of rain water harvesting, planting more trees and other measures that the general public can take to fight drought. This is a good way to spread awareness and control the problem.

Though the government has put certain drought relief plans in place however these are not enough to overcome the drastic problem of drought. It is important to take strong steps to avoid this problem. Everyone should contribute their bit to control this problem.

Related Information:

• Essay on Flood
• Paragraph on Flood

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The Drought Essay Questions

By j.g. ballard, essay questions.

These notes were contributed by members of the GradeSaver community. We are thankful for their contributions and encourage you to make your own.

Written by people who wish to remain anonymous

Why has water become scarce in the world of The Drought ?

In the world of The Drought , water has become scarce because of climate change brought about by human actions. Specifically, the effects of rapid industrialization and the waste created by said industrial activity destroy the precipitation cycle, prevent evaporation from occurring, cause the ocean to retreat, and turn the areas left behind by the oceans into vast, hot deserts. Because the water was poisoned and is retreating, water becomes very scarce in the world, which kills quite a few people and causes those who remain to fight tooth and nail over what little water remains.

Before the drought began, what did Ransom do for work?

Before the drought began, Ransom (the protagonist of the novel) was a medical doctor. Readers never learn what kind of doctor Ransom was; instead, his ability (or lack thereof) as a medical practitioner is left up to readers' inferences. However, many of the characters in the novel refuse to ask for—or follow—Ransom's advice. They still call him "doctor," though, indicating that they respect him.

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The Drought Questions and Answers

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Study Guide for The Drought

The Drought study guide contains a biography of J.G. Ballard, literature essays, quiz questions, major themes, characters, and a full summary and analysis.

• About The Drought
• The Drought Summary
• Character List

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Guest Essay

I’m a Scientist in California. Here’s What Worries Me Most About Drought.

By Andrew Schwartz

Dr. Schwartz is the lead scientist and station manager at the University of California, Berkeley, Central Sierra Snow Lab.

Outside my lab near Donner Pass in the Sierra Nevada of California, new animal tracks are on the snow after a winter of hibernation, bird songs are lofting through the air, and the creek is flowing strongly with water from the melting snow. Spring has come worryingly early to the Sierra Nevada.

This past week, I joined teams of other scientists gathering the most important measurements of the Sierra Nevada snowpack from over 265 sites throughout the state. Typically, this measurement marks the transition from snow accumulation season to the melt season and contains the most snow of any measurement throughout the year. The 2022 results, however, confirmed what those of us monitoring the state’s drought had feared: California’s snowpack is now at 39 percent of its average, or 23 percent lower than at the same point last year. This signals a deepening of the drought — already the worst in the western United States in 1,200 years — and another potentially catastrophic fire season for much of the West.

Many people have a rather simplistic view of drought as a lack of rain and snow. That’s accurate — to an extent. What it doesn’t account for is human activity and climate change that are now dramatically affecting the available water and its management. As more frequent and large wildfires and extended dry periods batter the land, our most important tools for managing water are becoming less and less accurate. At the same time, our reliance on these models to try to make the most of the little water we have is becoming more and more problematic.

Droughts may last for several years or even over a decade, with varying degrees of severity. During these types of extended droughts, soil can become so dry that it soaks up all new water, which reduces runoff to streams and reservoirs. Soil can also become so dry that the surface becomes hard and repels water, which can cause rainwater to pour off the land quickly and cause flooding. This means we no longer can rely on relatively short periods of rain or snow to completely relieve drought conditions the way we did with past droughts.

Many storms with near record-breaking amounts of rain or snow would be required in a single year to make a significant dent in drought conditions. October was the second-snowiest and December the snowiest month on record at the snow lab since 1970, thanks to two atmospheric rivers that hit California. But the exceptionally dry November and January to March periods have left us with another year of below-average snowpack, rain and runoff conditions.

This type of feast-or-famine winter with big storms and long, severe dry periods is expected to increase as climate change continues . As a result, we’ll need multiple above-average rain and snow years to make up the difference rather than consecutive large events in a single year.

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National Integrated Drought Information System

counties with USDA Drought Disaster Designations (primary)

Idaho residents in areas of drought, according to the Drought Monitor

driest July on record (since 1895)

driest January—July on record (since 1895)

The U.S. Drought Monitor depicts the location and intensity of drought across the country. The map uses 5 classifications: Abnormally Dry (D0), showing areas that may be going into or are coming out of drought, and four levels of drought (D1–D4).

This map is used by the U.S. Department of Agriculture to trigger some disaster declarations and loan eligibility. Individual states and water supply planning may use additional information to inform their declarations and actions. Learn more .

How has drought impacted this state in the past? View examples of past drought impacts  or explore historical Drought Monitor maps .

The U.S. Drought Monitor 1-week change map shows where drought has improved, remained the same, or worsened since the previous week's Drought Monitor. 

The U.S. Drought Monitor depicts the location and intensity of drought across the country, using 5 classifications (D0–D4). Green hues indicate conditions improved, while yellow/orange hues indicate degradations.

The Multi-Indicator Drought Index (MIDI) looks at current drought conditions across the U.S. by integrating several key drought indices on precipitation and moisture into one objective, computer-generated map. 

The Short-Term MIDI approximates  drought impacts from changes in precipitation and moisture  over a short-term timeframe (looking back up to 90 days), such as impacts to non-irrigated agriculture, topsoil moisture, and range and pasture conditions.  Long-term droughts  (lasting months to years) can have different impacts.

This experimental map is based on methodology from the NOAA National Weather Service’s Climate Prediction Center. Learn  how this map is made .

The Long-Term MIDI approximates  drought impacts from changes in precipitation and moisture  over a long-term timeframe (up to 5 years), such as impacts to irrigated agriculture, groundwater, and reservoir levels.  Long-term drought  conditions can also increase wildfire intensity and severity.

A  drought index  combines multiple drought indicators (e.g., precipitation, temperature, soil moisture) to depict drought conditions. For some products, like the U.S. Drought Monitor, authors combine their analysis of drought indicators with input from local observers. Other drought indices, like the Standardized Precipitation Index (SPI), use an objective calculation to describe the severity, location, timing, and/or duration of drought. 

Periods of drought can lead to inadequate  water supply , threatening the health, safety, and welfare of communities. Streamflow, groundwater, reservoir, and snowpack data are key to monitoring and forecasting water supply.

Drought can reduce the water availability and water quality necessary for productive farms, ranches, and grazing lands, resulting in significant negative direct and indirect economic impacts to the agricultural sector. Monitoring  agricultural drought typically focuses on examining levels of precipitation, evaporative demand, soil moisture, and surface/groundwater quantity and quality.

Drought is defined as the lack of precipitation over an extended period of time, usually for a season or more, that results in a water shortage. Changes in precipitation can substantially disrupt crops and livestock, influence the frequency and intensity of severe weather events, and affect the quality and quantity of water available for municipal and industrial use.

Drought & Dryness Categories

Abnormally dry.

Abnormally Dry (D0) indicates a region that is going into or coming out of drought.  View typical impacts by state , or learn how Idaho contributes to the U.S. Drought Monitor .

Moderate Drought

Moderate Drought (D1) is the first of four drought categories (D1–D4), according to the U.S. Drought Monitor.  View typical impacts by state , or learn how Idaho contributes to the U.S. Drought Monitor .

Severe Drought

Severe Drought (D2) is the second of four drought categories (D1–D4), according to the U.S. Drought Monitor.  View typical impacts by state , or learn how Idaho contributes to the U.S. Drought Monitor .

Extreme Drought

Extreme Drought (D3) is the third of four drought categories (D1–D4), according to the U.S. Drought Monitor.  View typical impacts by state , or learn how Idaho contributes to the U.S. Drought Monitor .

Exceptional Drought

Exceptional Drought (D4) is the most intense drought category, according to the U.S. Drought Monitor.  View typical impacts by state , or learn how Idaho contributes to the U.S. Drought Monitor .

Total Area in Drought (D1–D4)

The percent area of Idaho that is currently in drought (D1–D4), according to the U.S. Drought Monitor. Learn how Idaho contributes to the U.S. Drought Monitor .

Drought Change Since Last Week

3-category degradation.

Drought/dryness has worsened by 3 categories, according to the U.S. Drought Monitor.

2-Category Degradation

Drought/dryness has worsened by 2 categories, according to the U.S. Drought Monitor.

1-Category Degradation

Drought/dryness has worsened by 1 category, according to the U.S. Drought Monitor.

There has been no change in drought conditions at this location.

1-Category Improvement

Drought/dryness has improved by 1 category, according to the U.S. Drought Monitor.

2-Category Improvement

Drought/dryness has improved by 2 categories, according to the U.S. Drought Monitor.

3-Category Improvement

Drought/dryness has improved by 3 categories, according to the U.S. Drought Monitor.

Dry Conditions

D4: exceptional drought.

This map integrates multiple drought indices measuring precipitation and moisture into one computer-generated drought map, with a reference period of 1979–present. According to these indices, current conditions are drier than 98% to 100% of past conditions.  Learn more about these categories .

D3: Extreme Drought

This map integrates multiple drought indices measuring precipitation and moisture into one computer-generated drought map, with a reference period of 1979–present. According to these indices, current conditions are drier than 95% to 98% of past conditions.  Learn more about these categories .

D2: Severe Drought

This map integrates multiple drought indices measuring precipitation and moisture into one computer-generated drought map, with a reference period of 1979–present. According to these indices, current conditions are drier than 90% to 95% of past conditions.  Learn more about these categories .

D1: Moderate Drought

This map integrates multiple drought indices measuring precipitation and moisture into one computer-generated drought map, with a reference period of 1979–present. According to these indices, current conditions are drier than 80% to 90% of past conditions.  Learn more about these categories .

D0: Abnormally Dry

This map integrates multiple drought indices measuring precipitation and moisture into one computer-generated drought map, with a reference period of 1979–present. According to these indices, current conditions are drier than 70% to 80% of past conditions.  Learn more about these categories .

Wet Conditions

W0: abnormally wet.

This map integrates multiple drought indices measuring precipitation and moisture into one computer-generated drought map, with a reference period of 1979–present. According to these indices, current conditions are wetter than 70% to 80% of past conditions.  Learn more about these categories .

W1: Moderate Wet

This map integrates multiple drought indices measuring precipitation and moisture into one computer-generated drought map, with a reference period of 1979–present. According to these indices, current conditions are wetter than 80% to 90% of past conditions.  Learn more about these categories .

W2: Severe Wet

This map integrates multiple drought indices measuring precipitation and moisture into one computer-generated drought map, with a reference period of 1979–present. According to these indices, current conditions are wetter than 90% to 95% of past conditions.  Learn more about these categories .

W3: Extreme Wet

This map integrates multiple drought indices measuring precipitation and moisture into one computer-generated drought map, with a reference period of 1979–present. According to these indices, current conditions are wetter than 95% to 98% of past conditions.  Learn more about these categories .

W4: Exceptional Wet

This map integrates multiple drought indices measuring precipitation and moisture into one computer-generated drought map, with a reference period of 1979–present. According to these indices, current conditions are wetter than 98% to 100% of past conditions.  Learn more about these categories .

This map is released every Thursday morning, with data valid through Tuesday at 7am Eastern.

U.S. Drought Monitor change maps are released every Thursday morning, with data valid through Tuesday at 7 am Eastern.

The drought indices used in this map are based on the GridMET dataset and use a reference period of 1979–present. This map is updated every 5 days, with a delay of 4 to 5 days to allow for data collection and quality control.

Drought in the Pacific Northwest

Drought and its impacts vary from region to region—due to differences in climate. The Pacific Northwest is an ecologically diverse region where water supplies are heavily reliant on snowpack, precipitation, and groundwater, as well as on highly managed rivers, like the Columbia River. Despite its soggy reputation, the region is primarily wet in the winter but dry in the summer, and has experienced multiple droughts in the early 21st century—impacting agriculture, water supply, hydropower, tourism and recreation, fisheries, and wildland fire regimes. Recently, in 2001, 2015, and 2021, virtually the entire region experienced significant drought. In 2015 historic levels of drought were experienced across western Washington and Oregon. Over the last several years, while the coastal regions experienced an unprecedented single-year drought, central and southern Oregon and Idaho suffered under a prolonged, multi-year drought. In response to drought in the region, NOAA’s National Integrated Drought Information System (NIDIS) launched the Pacific Northwest Drought Early Warning System (DEWS) in 2016, encompassing Idaho, Oregon, Washington, and western Montana. The Pacific Northwest DEWS is a network of regional and national partners that share information and coordinate actions to help communities in the region cope with drought. Reach out to Jason Gerlich , the Regional Drought Coordinator for this region, for more information, or sign up for the Pacific Northwest DEWS newsletter.

Idaho State Drought Resources

State Drought Website:

Idaho Department of Water Resources | State Drought Declarations

State Drought Agency:  

Idaho Department of Water Resources

State Drought & Hazard Mitigation Plans:

State of Idaho 2023 Hazard Mitigation Plan

t Idaho Drought Plan (2001)

State Climate Office: 

Idaho Climate Services

Other Resources:

2023 Pacific Northwest Water Year Impacts Assessment

Idaho Current Conditions

A number of physical indicators are important for monitoring drought, such as precipitation & temperature, water supply (e.g., streamflow, reservoirs), and soil moisture. Learn more about monitoring drought .

Idaho Precipitation Conditions

Inches of precipitation.

This location received less than 0.01 inch of precipitation during this 7-day period.

This location received  0.01–0.5 inch of precipitation during this 7-day period.

This location received  0.5–1 inch of precipitation during this 7-day period.

This location received  1–2 inches of precipitation during this 7-day period.

This location received  2–4 inches of precipitation during this 7-day period.

This location received  4–6 inches of precipitation during this 7-day period.

This location received  6–8 inches of precipitation during this 7-day period.

This location received  more than 8 inches of precipitation during this 7-day period.

Percent of Normal Precipitation (%)

<25% of normal.

Precipitation was only 0% to 25% of the historical average for this location, compared to the same date range from 1991–2020. 

25%–50% of Normal

Precipitation was 25% to 50% of the historical average for this location, compared to the same date range from 1991–2020. 

50%–75% of Normal

Precipitation was 50% to 75% of the historical average for this location, compared to the same date range from 1991–2020. 

75%–100% of Normal

Precipitation was 75% to 100% of the historical average for this location, compared to the same date range from 1991–2020. 

100%–150% of Normal

Precipitation was 100% to 150% of the historical average for this location, compared to the same date range from 1991–2020. 

150%–200% of Normal

Precipitation was 150% to 200% of the historical average for this location, compared to the same date range from 1991–2020. 

200%–300% of Normal

Precipitation was 200% to 300% of the historical average for this location, compared to the same date range from 1991–2020. 

>300% of Normal

Precipitation was greater than 300% of the historical average for this location, compared to the same date range from 1991–2020. 

This map shows total precipitation (in inches) for the past 7 days. Dark blue shades indicate the highest precipitation amounts.

This map shows precipitation for the past 30 days as a percentage of the historical average (1991–2020) for the same time period. Green/blue shades indicate above-normal precipitation, while brown shades indicate below-normal precipitation. 

This map shows precipitation for the past 60 days as a percentage of the historical average (1991–2020) for the same time period. Green/blue shades indicate above-normal precipitation, while brown shades indicate below-normal precipitation. 

Precipitation data are updated daily, with a delay of 3 to 4 days to allow for data collection and quality control.

Idaho Temperature Conditions

Maximum temperature (°f).

The 7-day average daily maximum temperature is below 0°F .

The 7-day average daily maximum temperature is between  0–10°F .

The 7-day average daily maximum temperature is between  1 0–20°F .

The 7-day average daily maximum temperature is between  2 0–30°F .

The 7-day average daily maximum temperature is between  3 0–40°F .

The 7-day average daily maximum temperature is between  4 0–60°F .

The 7-day average daily maximum temperature is between  6 0 –70°F .

The 7-day average daily maximum temperature is between  7 0 –80°F .

The 7-day average daily maximum temperature is between  8 0 –90°F .

The 7-day average daily maximum temperature is between  9 0 –100°F .

The 7-day average daily maximum temperature is between  greater than  1 00°F .

Departure from Normal Max Temperature (°F)

>8°f below normal.

The average maximum temperature was more than 8°F colder than normal for this location.

6–8°F Below Normal

The average maximum temperature was  6–8°F colder than normal for this location.

4–6°F Below Normal

The average maximum temperature was  4–6°F colder than normal for this location.

3–4°F Below Normal

The average maximum temperature was  3–4°F colder than normal for this location.

1–3°F Below Normal

The average maximum temperature was  1–3°F colder than normal for this location.

0–1°F Below Normal

The average maximum temperature was  0–1°F colder than normal for this location.

0–1°F Above Normal

The average maximum temperature was  0–1°F warmer than normal for this location.

1–3°F Above Normal

The average maximum temperature was  1–3°F warmer than normal for this location.

3–4°F Above Normal

The average maximum temperature was  3–4°F warmer than normal for this location.

4–6°F Above Normal

The average maximum temperature was  4–6°F warmer than normal for this location.

6–8°F Above Normal

The average maximum temperature was  6–8°F warmer than normal for this location.

>8°F Above Normal

The average maximum temperature was  more than 8°F warmer than normal for this location.

This map shows the average maximum daily temperature (°F) for the last 7 days. Blue hues indicate cooler temperatures, while red hues indicate warmer temperatures.

This map shows the average maximum daily temperature for the past 7 days compared to the historical average (1991–2020) for the same 7 days. Negative values ( blue hues ) indicate colder than normal temperatures, and positive values ( red hues ) indicate warmer than normal temperatures.

This map shows the average maximum daily temperature for the past 30 days compared to the historical average (1991–2020) for the same 30 days. Negative values ( blue hues ) indicate colder than normal temperatures, and positive values ( red hues ) indicate warmer than normal temperatures.

Temperature data are updated daily, with a delay of 3 to 4 days to allow for data collection and quality control.

Air  temperature can have wide-ranging effects on natural processes. Warmer air temperatures increase evapotranspiration—which is the combination of evaporation from the soil and bodies of water and transpiration from plants—and lower soil moisture.

Idaho Streamflow Conditions

Streamflow conditions.

Estimated streamflow is the lowest value recorded at this gauge on this day of the year.  Learn more .

Much Below Normal (<10th Percentile)

Estimated streamflow is in the 0–10th percentile of historical streamflow values recorded at this gauge on this day of the year.  Learn more .

Below Normal (10th–25th Percentile)

Estimated streamflow is in the 10th–25th percentile of historical streamflow values recorded at this gauge on this day of the year.  Learn more .

Normal (25th–75th Percentile)

Estimated streamflow is in the 25th–75th percentile of historical streamflow values recorded at this gauge on this day of the year.  Learn more .

Above Normal (75th–90th Percentile)

Estimated streamflow is in the 75th–90th percentile of historical streamflow values recorded at this gauge on this day of the year.  Learn more .

Much Above Normal (>90th Percentile)

Estimated streamflow is in the 90th–100th percentile of historical streamflow values recorded at this gauge on this day of the year.  Learn more .

Record High

Estimated streamflow is the highest value ever measured at this gauge on this day of the year.  Learn more .

A flow category has not been computed for this gauge, for example due to insufficient historical data or no current streamflow estimates.

This map shows current streamflow conditions compared to historical conditions for the same day of the year. Click on a streamgage to view current data from the U.S. Geological Survey.

This map shows streamflow conditions averaged over the last 7 days, compared to historical conditions for the same time period. Click on a streamgage to view current data from the U.S. Geological Survey.

This map shows streamflow conditions averaged over the last 28 days, compared to historical conditions for the same time period. Click on a streamgage to view current data from the U.S. Geological Survey.

This map updates daily on Drought.gov. View the most recent real-time streamflow data via USGS .

Drought can alter the ecological balance of natural systems and harm fish, wildlife, and plant species, as well as the benefits that these ecosystems provide to human communities. The environmental consequences of drought include losses in plant growth; increases in fire and insect outbreaks; altered rates of carbon, nutrient, and water cycling; and local species extinctions.

Because energy and water are so interdependent, the availability and predictability of water resources can directly affect energy systems. Energy professionals need information on current drought conditions and outlooks in order to make informed decisions on cooling, alternative water supplies, pricing, and infrastructure security.

During drought conditions that result in low water levels on rivers and other waterways, port and maritime  navigation and transportation operations may be limited due to a reduction in available routes and cargo-carrying capacity, resulting in increased costs. In addition, higher temperatures that often coexist with drought can impact roads, airport runways, and rail lines.

Idaho Soil Moisture Conditions

20 cm soil moisture percentile, 0–2nd percentile.

Soil moisture at 20cm depth is in the bottom 2% (0–2nd percentile) of historical measurements for this day of the year. 

2nd–5th Percentile

Soil moisture at 20cm depth falls between the 2nd to 5th percentile of historical measurements for this day of the year.

5th–10th Percentile

Soil moisture at 20cm depth falls between the 5th to 10th percentile of historical measurements for this day of the year. 

10th–20th Percentile

Soil moisture at 20cm depth falls between the 10th to 20th percentile of historical measurements for this day of the year.

20th–30th Percentile

Soil moisture at 20cm depth falls between the 20th to 30th percentile of historical measurements for this day of the year.

30th–70th Percentile

Soil moisture at 20cm depth falls between the 30th to 70th percentile of historical measurements for this day of the year.

70th–80th Percentile

Soil moisture at 20cm depth falls between the 70th to 80th percentile of historical measurements for this day of the year. 

80th–90th Percentile

Soil moisture at 20cm depth falls between the 80th to 90th percentile of historical measurements for this day of the year.

90th–95th Percentile

Soil moisture at 20cm depth falls between the 90th to 95th percentile of historical measurements for this day of the year. 

95th–98th Percentile

Soil moisture at 20cm depth falls between the 95th to 98th percentile of historical measurements for this day of the year. 

98th–100th Percentile

Soil moisture at 20cm depth is in the top 2% ( 98th to 100th percentile) of historical measurements for this day of the year. 

0–100 cm Soil Moisture Percentile

Soil moisture at 0–100cm depth is in the bottom 2% (0–2nd percentile) of historical measurements for this day of the year. Learn more .

Soil moisture at 0–100cm depth falls between the 2nd to 5th percentile of historical measurements for this day of the year. Learn more .

Soil moisture at 0–100cm depth falls between the 5th to 10th percentile of historical measurements for this day of the year. Learn more .

Soil moisture at 0–100cm depth falls between the 10th to 20th percentile of historical measurements for this day of the year. Learn more .

Soil moisture at 0–100cm depth falls between the 20th to 30th percentile of historical measurements for this day of the year. Learn more .

Soil moisture at 0–100cm depth falls between the 30th to 70th percentile of historical measurements for this day of the year. Learn more .

Soil moisture at 0–100cm depth falls between the 70th to 80th percentile of historical measurements for this day of the year. Learn more .

Soil moisture at 0–100cm depth falls between the 80th to 90th percentile of historical measurements for this day of the year. Learn more .

Soil moisture at 0–100cm depth falls between the 90th to 95th percentile of historical measurements for this day of the year. Learn more .

Soil moisture at 0–100cm depth falls between the 95th to 98th percentile of historical measurements for this day of the year. Learn more .

Soil moisture at 0–100cm depth is in the top 2% ( 98th to 100th percentile) of historical measurements for this day of the year. Learn more .

This map shows the moisture content of the top 20 cm of soil compared to historical conditions, based on  in situ (in the ground) measurements of soil moisture. Red and orange hues indicate drier soils, while greens and blues indicate greater soil moisture.

This NASA  SPoRT-LIS  soil moisture  map shows the moisture content of the top 100 cm of soil compared to historical conditions (1981–2013), based on the Noah unified land surface model. Red and orange hues indicate drier soils, while greens and blues indicate greater soil moisture.

Soil moisture data are updated daily, with a 1-day delay due to differences in network report timing.

This map updates daily with data from NASA's Short-term Prediction and Transition Center – Land Information System ( SPoRT-LIS ).

Soil moisture plays an important role in drought and flood forecasting, agricultural monitoring, forest fire prediction, water supply management, and other natural resource activities. Soil moisture observations can forewarn of impending drought or flood conditions before other more standard indicators are triggered.

Flash drought  is the rapid onset or intensification of drought. Unlike slow-evolving drought, which is caused by a decline in precipitation, flash drought occurs when low precipitation is accompanied by abnormally high temperatures, high winds, and/or changes in radiation. These sometimes-rapid changes can quickly raise evapotranspiration rates and remove available water from the landscape.

Drought can result in reduced growth rates, increased stress on  vegetation , and alterations or transformations to the plant community and/or the entire ecosystem. During periods of drought, plants increase their demand for water through increased evapotranspiration and longer growing seasons. 

Outlooks & Forecasts for Idaho

Predicting drought in Idaho depends on the ability to forecast precipitation and temperature within the context of complex climate interactions. View more outlooks & forecasts .

Future Precipitation & Temperature Conditions

Predicted inches of precipitation, less than 0.01 inch, 0.01 to 0.1 inch, 0.1 to 0.25 inch, 0.25 to 0.5 inch, 0.5 to 0.75 inch, 0.75 to 1 inch, 1 to 1.25 inches, 1.25 to 1.5 inches, 1.5 to 1.75 inches, 1.75 to 2 inches, 1.5 to 2 inches, 2 to 2.5 inches, 2.5 to 3 inches, 3 to 4 inches, 4 to 5 inches, 5 to 7 inches, 7 to 10 inches, 10 to 15 inches, 15 to 20 inches, more than 20 inches, probability of below-normal precipitation, 33%–40% chance of below normal.

There is an 33%–40% chance  of below-normal precipitation during this period. 

40%–50% Chance of Below Normal

There is an 40%–50% chance  of below-normal precipitation during this period. 

50%–60% Chance of Below Normal

There is an 50%–60% chance  of below-normal precipitation during this period. 

60%–70% Chance of Below Normal

There is an 60%–70% chance  of below-normal precipitation during this period. 

70%–80% Chance of Below Normal

There is an 70%–80% chance  of below-normal precipitation during this period. 

80%–90% Chance of Below Normal

There is an 80%–90% chance  of below-normal precipitation during this period. 

>90% Chance of Below Normal

There is a >90% chance  of below-normal precipitation during this period. 

Probability of Above-Normal Precipitation

33%–40% chance of above normal.

There is an 33%–40% chance  of above-normal precipitation during this period. 

40%–50% Chance of Above Normal

There is an 40%–50% chance  of above-normal precipitation during this period. 

50%–60% Chance of Above Normal

There is an 50%–60% chance  of above-normal precipitation during this period. 

60%–70% Chance of Above Normal

There is an 60%–70% chance  of above-normal precipitation during this period. 

70%–80% Chance of Above Normal

There is an 70%–80% chance  of above-normal precipitation during this period. 

80%–90% Chance of Above Normal

There is an 80%–90% chance  of above-normal precipitation during this period. 

>90% Chance of Above Normal

There is a  >90% chance  of above-normal precipitation during this period. 

Near-Normal

Odds favor near-normal precipitation during this period.

Probability of Below-Normal Temperatures

There is an 33%–40% chance  of below-normal temperatures during this period. 

There is an 40%–50% chance  of below-normal temperatures during this period. 

There is an 50%–60% chance  of below-normal temperatures during this period. 

There is an 60%–70% chance  of below-normal temperatures during this period. 

There is an 70%–80% chance  of below-normal temperatures during this period. 

There is an 80%–90% chance  of below-normal temperatures during this period. 

There is a >90% chance  of below-normal temperatures during this period. 

Probability of Above-Normal Temperatures

There is an 33%–40% chance  of above-normal temperatures during this period. 

There is an 40%–50% chance  of above-normal temperatures during this period. 

There is an 50%–60% chance  of above-normal temperatures during this period. 

There is an 60%–70% chance  of above-normal temperatures during this period. 

There is an 70%–80% chance  of above-normal temperatures during this period. 

There is an 80%–90% chance  of above-normal temperatures during this period. 

There is a  >90% chance  of above-normal temperatures during this period. 

Odds favor near-normal temperatures during this period.

This map shows the amount of liquid precipitation (in inches) expected to fall over the next 7 days, according to the National Weather Service.

This map shows the probability (percent chance) of above-normal, near-normal, or below-normal precipitation 8 to 14 days in the future.

This map shows the probability (percent chance) of above-normal, near-normal, or below-normal temperature 8 to 14 days in the future.

The Quantitative Precipitation Forecast maps on Drought.gov are updated once a day and are valid from 7 a.m. Eastern that day.

The Climate Prediction Center updates their 8–14 day outlooks daily.

Drought Outlooks for Idaho

Drought is predicted to..., drought persists.

During this time period,  NOAA's Climate Prediction Center predicts that drought conditions will persist.

Drought Improves

During this time period, NOAA's Climate Prediction Center predicts that existing drought conditions will improve (but not be removed).

Drought Is Removed

During this time period, NOAA's Climate Prediction Center predicts that drought will be removed.

Drought Develops

During this time period, NOAA's Climate Prediction Center predicts that drought will develop.

No Drought Present

According to NOAA's Climate Prediction Center, there is no drought, and is drought development is not predicted.

The Monthly Drought Outlook predicts whether drought will develop, remain, improve, or be removed in the next calendar month. 

The Seasonal Drought Outlook predicts whether drought will develop, remain, improve, or be removed in the next 3 months or so.

The Climate Prediction Center issues its Monthly Drought Outlooks on the last day of the calendar month.

The Climate Prediction Center issues its Seasonal Drought Outlooks on the third Thursday of each calendar month. Sometimes, the map is adjusted on the last day of the month to maintain consistency with the Monthly Drought Outlook.

Snow drought  is a period of abnormally low snowpack for the time of year. Snowpack typically acts as a natural reservoir, providing water throughout the drier summer months. Lack of snowpack storage, or a shift in timing of snowmelt, can be a challenge for drought planning. 

During drought conditions, fuels for  wildfire , such as grasses and trees, can dry out and become more flammable. Drought can also increase the probability of ignition and the rate at which fire spreads. Temperature, soil moisture, humidity, wind speed, and fuel availability (vegetation) are all factors that interact to influence the frequency of large wildfires.

Historical Drought Conditions in Idaho

Drought is a normal climate pattern that has occurred in varying degrees of length, severity, and size throughout history. Below, you can look back at past drought conditions for Idaho according to 3 historical drought indices. The U.S. Drought Monitor is a weekly map that shows the location and intensity of drought across the country since 2000. The Standardized Precipitation Index (SPI) is a monthly depiction of drought based on precipitation (with data going back to 1895). And the paleoclimate data uses tree-ring reconstructions to estimate drought conditions before we had widespread instrumental records, going back to the year 0 for some parts of the U.S.  View more historical conditions .

U.S. Drought Monitor

D0 - abnormally dry.

Abnormally Dry (D0) indicates a region that is going into or coming out of drought, according to the U.S. Drought Monitor.  View typical impacts by state.

D1 – Moderate Drought

Moderate Drought (D1) is the first of four drought categories (D1–D4), according to the U.S. Drought Monitor.  View typical impacts by state.

D2 – Severe Drought

Severe Drought (D2) is the second of four drought categories (D1–D4), according to the U.S. Drought Monitor.  View typical impacts by state.

D3 – Extreme Drought

Extreme Drought (D3) is the third of four drought categories (D1–D4), according to the U.S. Drought Monitor. View typical impacts by state.

D4 – Exceptional Drought

Exceptional Drought (D4) is the most intense drought category, according to the U.S. Drought Monitor.  View typical impacts by state.

The U.S. Drought Monitor (2000–present) depicts the location and intensity of drought across the country. Every Thursday, authors from NOAA, USDA, and the National Drought Mitigation Center produce a new map based on their assessments of the best available data and input from local observers. The map uses five categories: Abnormally Dry (D0), showing areas that may be going into or are coming out of drought, and four levels of drought (D1–D4).  Learn more .

D4 (SPI of -2.0 or less)

The 9-month Standardized Precipitation Index (SPI) value for this location is -2.0 or less , indicating exceptional drought (D4) conditions.

D3 (SPI of -1.9 to -1.6)

The Standardized Precipitation Index (SPI) value for this location is between -1.9 to -1.6 , indicating extreme drought (D3) conditions.

D2 (SPI of -1.5 to -1.3)

The Standardized Precipitation Index (SPI) value for this location is between -1.5 to -1.3 , indicating severe drought (D2) conditions.

D1 (SPI of -1.2 to -0.8)

The Standardized Precipitation Index (SPI) value for this location is between -1.2 to -0.8 , indicating moderate drought (D1) conditions.

D0 (SPI of -0.7 to -0.5)

The Standardized Precipitation Index (SPI) value for this location is between -0.7 to -0.5 , indicating abnormally dry (D0) conditions.

W0 (SPI of 0.5 to 0.7)

The Standardized Precipitation Index (SPI) value for this location is between 0.5 to 0.7 , indicating abnormally wet (W0) conditions.

W1 (SPI of 0.8 to 1.2)

The Standardized Precipitation Index (SPI) value for this location is between 0.8 to 1.2 , indicating moderate wet (W1) conditions.

W2 (SPI of 1.3 to 1.5)

The Standardized Precipitation Index (SPI) value for this location is between 1.3 to 1.5 , indicating severe wet (W2) conditions.

W3 (SPI of 1.6 to 1.9)

The Standardized Precipitation Index (SPI) value for this location is between 1.6 to 1.9 , indicating extreme wet (W3) conditions.

W4 (SPI of 2.0 or more)

The Standardized Precipitation Index (SPI) value for this location is  2.0 or greater , indicating exceptional wet (W4) conditions.

Drought results from an imbalance between water supply and water demand. The Standardized Precipitation Index (SPI) measures water supply, specifically precipitation. SPI captures how observed precipitation (rain, hail, snow) deviates from the climatological average over a given time period—in this case, over the 9 months leading up to the selected date. Red hues indicate drier conditions, while blue hues indicate wetter conditions. Data are available monthly from 1895–present. 

D4 (PMDI of -5.0 or less)

Tree rings were used to reconstruct a Palmer Modified Drought Index (PMDI) value for each June–August, estimating relative dryness. The PMDI value for this location is -5.0 or less , indicating exceptional drought (D4) conditions.

D3 (PMDI of -4.9 to -4.0)

Tree rings were used to reconstruct a Palmer Modified Drought Index (PMDI) value for each June–August, estimating relative dryness. The PMDI value for this location is -4.9 to -4.0 , indicating extreme drought (D3) conditions.

D2 (PMDI of -3.9 to -3.0)

Tree rings were used to reconstruct a Palmer Modified Drought Index (PMDI) value for each June–August, estimating relative dryness. The PMDI value for this location is -3.9 to -3.0 , indicating severe drought (D2) conditions.

D1 (PMDI of -2.9 to -2.0)

Tree rings were used to reconstruct a Palmer Modified Drought Index (PMDI) value for each June–August, estimating relative dryness. The PMDI value for this location is -2.9 to -2.0 , indicating moderate drought (D1) conditions.

D0 (PMDI of -1.9 to -1.0)

Tree rings were used to reconstruct a Palmer Modified Drought Index (PMDI) value for each June–August, estimating relative dryness. The PMDI value for this location is -1.9 to -1.0 , indicating abnormally dry (D0) conditions.

W0 (PMDI of 1.0 to 1.9)

Tree rings were used to reconstruct a Palmer Modified Drought Index (PMDI) value for each June–August, estimating relative dryness. The PMDI value for this location is 1.0 to 1.9 , indicating abnormally wet (W0) conditions.

W1 (PMDI of 2.0 to 2.9)

Tree rings were used to reconstruct a Palmer Modified Drought Index (PMDI) value for each June–August, estimating relative dryness. The PMDI value for this location is 2.0 to 2.9 , indicating moderate wet (W1) conditions.

W2 (PMDI of 3.0 to 3.9)

Tree rings were used to reconstruct a Palmer Modified Drought Index (PMDI) value for each June–August, estimating relative dryness. The PMDI value for this location is 3.0 to 3.9 , indicating severe wet (W2) conditions.

W3 (PMDI of 4.0 to 4.9)

Tree rings were used to reconstruct a Palmer Modified Drought Index (PMDI) value for each June–August, estimating relative dryness. The PMDI value for this location is 4.0 to 4.9 , indicating extreme wet (W3) conditions.

W4 (PMDI of 5.0 or greater)

Tree rings were used to reconstruct a Palmer Modified Drought Index (PMDI) value for each June–August, estimating relative dryness. The PMDI value for this location is 5.0 or greater , indicating exceptional wet (W4) conditions.

In paleoclimatology, proxy climate data (e.g., tree rings, ocean sediments) can allow us to reconstruct past climate conditions before we had widespread instrumental records. The Living Blended Drought Atlas , shown here, estimates average drought conditions each summer (June–August) as far back as the year 0 by combining tree-ring reconstructions and instrumental records. Red hues indicate drier conditions, while blue hues indicate wetter conditions.

Drought Resources for Idaho

Stay informed: local drought updates.

Drought Alert Emails Get email updates when U.S. Drought Monitor conditions change for your location or a new drought outlook is released.

Regional Drought Status Updates NIDIS & its partners issue regional updates covering drought conditions, outlooks/forecasts, and local impacts.

Pacific Northwest Drought Email List Get regional drought status updates right to your inbox, as well as drought news, webinars, and other events for the Pacific Northwest.

Pacific Northwest DEWS Drought & Climate Outlook Webinars These webinars provide the region with timely information on current and developing drought conditions, as well as climatic events like El Niño and La Niña.

Drought in your area?  Tell us how drought is impacting your community by submitting a condition monitoring report. Your submissions help us better understand how drought is affecting local conditions.

State & Regional Resources

Idaho Drought Plan (2001)

MesoWest | Idaho

CoCoRaHS | Idaho

University of Idaho Extension | Drought Resources

NDMC | Idaho Drought Planning Resources

USDA Farm Service Agency | Idaho

USDA Natural Resources Conservation Service | Idaho Snow Survey

National Weather Service:

• Western Region Headquarters
• Northwest River Forecast Center (NWRFC)
• Colorado Basin River Forecast Center (CBRFC)
• OTX - Spokane, WA
• MSO - Missoula, MT
• BOI - Boise, ID
• PIH - Pocatello, ID

Western Regional Climate Center

USDA | Northwest Climate Hub

USDA Northwest Climate Hub & NDMC | Idaho & the U.S. Drought Monitor

Northwest Climate Adaptation Science Center

Northwest Climate Resilience Collaborative (NCRC, a NOAA CAP/RISA team)

Resources: Climate & Drought

Fifth National Climate Assessment | Chapter 27: Northwest

NOAA/NCEI | Idaho State Climate Summary

U.S. Climate Resilience Toolkit