• drought
    A cracked, parched landscape is often an effect of drought.

    Photograph by James L. Stanfield, National Geographic

    Yunnan Drought
    The ongoing drought in Yunnan Province, China, has forced some families to transport water from more than 10 kilometers (6 miles) away.
    Drought in the USA
    In August 2012, drought conditions extended over 70 percent of the United States. Counties in 33 states were designated “disaster counties” by the government. In the beginning of 2013, drought still affected more than 60 percent of the country.  
    Dust Bowl
    John Steinbeck’s 1939 novel The Grapes of Wrath describes the Dust Bowl drought of the 1930s: “Every moving thing lifted the dust into the air: a walking man lifted a thin layer as high as his waist, and a wagon lifted the dust as high as the fence tops, and an automobile boiled a cloud behind it. The dust was long in setting back again.”
    Comparing Natural Disasters
    • 2004 tsunami in Indonesia: affected 2 million people
    • 2010 earthquake in Haiti: affected 3 million people
    • Current drought/famine/war in the Horn of Africa: affecting 13 million people
    Drought is an extended period of unusually dry weather when there is not enough rain. The lack of precipitation can cause a variety of problems for local communities, including damage to crops and a shortage of drinking water. These effects can lead to devastating economic and social disasters, such as famine, forced migration away from drought-stricken areas, and conflict over remaining resources. 
     
    Because the full effects of a drought can develop slowly over time, impacts can be underestimated. However, drought can have drastic and long-term effects on vegetation, animals, and people. Since 1900, more than 11 million people have died and more than 2 billion people have been affected by drought. Drought is also one of the costliest weather-related disasters. In the past 30 years, the U.S. has experienced 16 billion-dollar droughts, totaling $195 billion in losses.  
     
    Defining Drought
     
    Drought is a complicated phenomenon, and can be hard to define. One difficulty is that drought means different things in different regions. "Drought" is not a set number or equation. It is defined depending on the average amount of precipitation an area is accustomed to receiving. 
     
    For example, in Atlanta, Georgia, the average rainfall is about 127 centimeters (50 inches) a year. If significantly less rain falls, there may be water shortages and a drought may be declared. However, arid regions, such as the deserts of the American Southwest, receive less than 8 centimeters (3 inches) of rainfall each year. A drought in Atlanta would be a very wet period in Phoenix, Arizona!  
     
    Determining the start of a drought can be tricky. Unlike many natural hazards that bring about sudden and dramatic results—such as earthquakes, tornadoes, and hurricanes—the onset of a drought can be gradual and subtle. It can take weeks, months, or even years for the full effects of long-term inadequate rainfall to become apparent. 
     
    The end of a drought can also be difficult to determine. While a single rainstorm will provide short-term relief from a drought, it might take weeks or months before levels of precipitation return to normal. The start and end of a drought are often only clear in hindsight.
     
    Causes of Drought
     
    Most droughts occur when regular weather patterns are interrupted, causing disruption to the water cycle. Changes in atmospheric circulation patterns can cause storm tracks to be stalled for months or years, dramatically impacting the amount of precipitation a region normally receives and resulting in droughts or floods. Changes in wind patterns can also affect how much moisture a region can absorb. 
     
    Scientists have found a link between certain climate patterns and drought. El Niño is a weather event where the surface water in the Pacific Ocean along the central South American coast rises in temperature. These warmer waters alter storm patterns and are associated with droughts in Indonesia, Australia, and northeastern South America. El Nino events are not predictable and can occur every two to seven years.
     
    La Niña is the counterpart to El Niño, when the surface water in the Pacific Ocean along the coast of South America decreases in temperature. The cooler waters affect storm patterns by contributing to drier-than-normal conditions in parts of North and South America. While El Niño usually lasts less than a year, La Niña can extend for one to three years. The effects of La Niña on weather patterns are often more complex than El Niño. Two of the most devastating droughts in the history of the United States—the 1930s Dust Bowl and the 1988 drought in the Midwest—are associated with the effects of La Niña.
     
    There is still a lot of debate about the connection between drought and global warming, the current period of climate change. A 2013 NASA study predicts warmer worldwide temperatures will mean increased rainfall in some parts of the world and decreased rainfall in others, leading to both more flooding and more droughts worldwide. Other scientists question the prediction that there will be more droughts and believe global warming will create a wetter climate around the world.  
     
    Impacts of Drought
     
    Trees and other plants have adapted to withstand the effects of drought through various survival methods. Some plants (such as grasses) will slow their growth or turn brown to conserve water. Trees can drop their leaves earlier in the season to prevent losing water through the leaf surface. However, if drought conditions persist, much vegetation will die.
     
    Certain plants have adapted so they can withstand long periods without water. Yuccas, for instance, have deep root systems that can seek out water with incredible efficiency. Cacti have spiny, hairy leaves that limit how much water they lose to evaporation. Mosses can withstand complete dehydration. Juniper trees can self-prune by steering water only toward the branches they need to survive. Other plants only grow when there is enough water to support them. In periods of drought, their seeds can survive under the soil for years until conditions are favorable again.
     
    However, many organisms cannot adapt to drought conditions, and the environmental effects of extended, unusual periods of low precipitation can be severe. Negative impacts include damage to habitats, loss of biodiversity, soil erosion, and an increased risk from wildfires. During the U.S. drought of 1988, rainfall in many states was 50 to 85 percent below normal. Summer thunderstorms produced lightning without rain and ignited fires in dry trees. More than 4 million acres of forest in the Northwest burned in a single summer. In Yellowstone National Park alone, 36 percent of the park was destroyed by fire. 
     
    Drought can also create significant economic and social problems. The lack of rain can result in crop loss, a decrease in land prices, and unemployment due to declines in production. As water levels in rivers and lakes fall, water-supply problems can develop. These can bring about other social problems. Many of these problems are health-related, such as lack of water, poor nutrition, and famine. Other problems include conflicts over water usage and food, and forced migration away from drought-stricken areas. 
     
    While drought is a naturally occurring part of the weather cycle and cannot be prevented, human activity can influence the effects that drought has on a region. Many modern agricultural practices may make land more vulnerable to drought. While new irrigation techniques have increased the amount of land that can be used for farming, they have also increased farmers’ dependence on water. 
     
    Traditional farming techniques allow land to “rest” by rotating crops each season and alternating areas where livestock graze. Now, with many areas in the world struggling with overpopulation and a shortage of farmland, there is often not enough arable land to support these sustainable farming practices. Over-farming and overgrazing can lead to soil being compacted and unable to hold water. As the soil becomes drier, it is vulnerable to erosion. This process can lead to fertile land becoming desert-like, a process known as desertification. The desertification of the Sahel in North Africa is partly blamed on a prolonged drought whose effects were intensified by farming practices that result in overgrazing.
     
    Increased drought conditions in Kenya have been attributed to deforestation and other human activities. Trees help bring precipitation into the ground and prevent soil erosion. But in 2009, it was reported that one-quarter of a protected forest reserve had been cleared for farming and logging, leading to drought conditions affecting 10 million people around the country. 
     
    Historical Droughts 
     
    Scientists often study historical droughts to put modern-day droughts in perspective. Since our data from thermometers and rain gauges only goes back about 100 to 150 years, scientists must research paleoclimatology, the study of the atmosphere of prehistoric Earth. Scientists gather paleoclimatic data from tree rings, sediments found in lakes and oceans, ice cores, and archaeological features and artifacts. This allows scientists to extend their understanding of weather patterns for millions of years in the past. 
     
    Analyzing paleoclimatic data shows that severe and extended droughts are an inevitable part of natural climate cycles. North America has experienced a number of long-lasting droughts with significant effects. It is thought that droughts brought about the decline of the Ancestral Puebloans in the Southwest during the 13th century, and the central and Lower Mississippian societies in the 14th to 16th centuries. 
     
    In South America, massive migration out of the once-fertile Atacama Desert 9,500 years ago can be explained by the onset of extreme drought.
     
    In Africa, the Sahel region experienced a series of droughts from 1400 to 1750 that radically altered the landscape. The water level in Lake Bosumtwi, Ghana, for instance, fell so low that an entire forest grew on the lake’s edges. Today, visitors can still see the tops of trees growing out of the lake—where the water is now more than 15 meters (50 feet) deep. 
     
    What scientists have learned by looking at Earth’s drought history is that periods of severe drought are a regular part of nature’s cycle. As devastating as droughts in the last century have been, they are considered relatively minor compared to the severity of earlier droughts that have lasted more than a century.
     
    Major Droughts in the Past Century
     
    The Dust Bowl of the 1930s is probably the most well-known drought experienced by the U.S. By 1934, 80 percent of the U.S. was struggling with moderate-to-severe drought conditions. The drought lasted nearly a decade and had devastating effects on crop production in the Great Plains. The combination of lack of rain, high temperatures, and strong winds affected more than 50 million acres of land. Massive clouds of dust and sand formed as unusually strong winds lifted the dry soil into the air. These clouds could block out the sun for days, giving the period the name “dust bowl.” In 1934, one dust cloud infamously traveled 2,414 kilometers (1,500 miles), from the Great Plains to the eastern U.S. 
     
    Mass migration was an indirect effect of the Dust Bowl. Farmers and their families were forced to migrate to other areas in search of work, and by 1940, 2.5 million people had fled the Great Plains. Of those, 200,000 moved to California. The influx of migrants into existing economies already strained by the Great Depression led to a rise in conflict, unemployment, and poverty.
     
    In the 1950s, severe drought returned to the Great Plains and southwestern United States, affecting half of the continental U.S. Low rainfall and high temperatures caused the production of crops in some areas to drop nearly 50 percent. Hay became too expensive for ranchers, and they had to feed their cattle prickly pear cactus and molasses to keep them alive. By the end of the five-year drought in 1957, 244 of Texas’ 254 counties had been declared federal drought disaster areas.  
     
    In the late 1980s, the U.S. experienced the costliest drought in its history. The three-year spell of high temperatures and low rainfall ruined roughly $15 billion of crops in the Corn Belt. The total of all the losses in energy, water, ecosystems, and agriculture is estimated at $39 billion. Federal assistance programs were able to help many farmers, but a longer-lasting drought would make it more difficult for the government to provide nationwide aid.
     
    Droughts continue to affect the U.S. Texas has been suffering from drought since 2010, with 2011 ranking as the driest year in the state’s history. A September 2012 National Geographic magazine article called Texas “The New Dust Bowl.” By 2013, 95 percent of the state was dealing with drought.  
     
    Australia is also a frequent victim of drought. The last decade has been especially severe, earning it the name The Big Dry or The Millennium Drought. Much of the country was placed under water restrictions, wildfires spread in the dry weather, and the water level in some dams fell to 25 percent.  In 2007, 65 percent of viable land in Australia was declared to be in a drought. The drought was officially declared over in April 2012.
     
    Droughts that occur in the developing world can cause even greater devastation. The Sahel region in Africa, which includes eight countries, endured a series of droughts in the 1970s and 1980s where annual rainfall dropped by 40 percent. In the early 1970s, more than 100,000 people died and millions of people were forced to migrate. Conditions continue to be critical in the area due to drought, overpopulation, failing crops, and high food prices. Drought emergencies for the region have been declared four times since 2000.   
     
    The Horn of Africa, which includes the countries of Ethiopia, Somalia, Eritrea, and Djibouti, is particularly vulnerable to droughts. Because almost 80 percent of the population is rural and depends on agriculture for food and income, famine often accompanies drought. 
     
    Struggles for the region’s limited, remaining resources can lead to conflict and war. In 1984 and 1985, the Horn of Africa suffered one of the worst droughts of the 20th century. The U.N. estimates that in Ethiopia alone, 1 million people died, 1.5 million livestock died, and 8.7 million people were affected by the drought—including being hospitalized, forced to migrate, or forced to change professions. In Sudan, 1 million people died, 7 million livestock died, and 7 million people were affected. 
     
    The cycle of drought-famine-conflict has persisted in the region, with drought conditions returning every few years since 2000. In 2006, drought affected 11 million people across the Horn of Africa, and in 2008-09, more than 20 million were affected. In 2011, drought and the resulting crisis killed between 50,000 and 100,000 people and affected more than 13 million.  
     
    Forecasting and Measuring Drought
     
    Even though scientists are unable to predict how long a drought will last or how severe it will be, early warning systems and monitoring tools can minimize some of drought’s damaging impacts. There are a number of tools used to monitor drought across the U.S. Due to the limitations of each system, data from different sources are often compiled to create a more comprehensive forecast
     
    The Palmer Drought Severity Index (PDSI), developed in 1965 by the National Weather Service, is the most commonly used drought monitor. It is a complex measurement system and an effective way to forecast long-term drought. Its limitations are that it does not provide early warnings for drought and is not as accurate for use in mountainous areas because it does not account for snow (only rain) as precipitation. The PDSI is often used by the U.S. Department of Agriculture to determine when to begin providing drought relief.
     
    Information from the Standardized Precipitation Index (SPI) is often used to supplement the PDSI data. The SPI, developed in 1993, is less complex than the PDSI and only measures precipitation—not evaporation or water runoff. Many scientists prefer using the SPI because the time period being analyzed can easily be customized. The SPI can also identify droughts many months earlier than the PDSI. The National Drought Mitigation Center uses the SPI to monitor drought conditions around the U.S.
     
    The U.S. Drought Monitor, started in 1999, is a joint effort between three U.S. government agencies—the Department of Agriculture, the Department of Commerce, and the National Oceanic and Atmospheric Administration (NOAA). The Monitor synthesizes data from academic and federal scientists into a weekly map indicating levels of dryness around the country. It is designed to be a blend of science and art that can be used as a general summary of drought conditions around the country. It is not meant to be used as a drought predictor or for detailed information about specific areas.
     
    The Famine Early Warning System Network (FEWS NET) monitors satellite data of crops and rainfall across Africa and some parts of Central America, the Middle East, and Central Asia. Analysis of the data allows for early intervention to try to prevent drought-induced famine.
     
    Preparing for Drought
     
    People and governments need to adopt new practices and policies to prepare as much as possible for inevitable future droughts. Emergency spending once a crisis has begun is less effective than money spent in preparation. The Federal Emergency Management Agency (FEMA) estimates that every $1 spent in planning for a natural hazard will save $4 in the long term.  
     
    Many areas are extremely vulnerable to drought as people continue to be dependent on a steady supply of water. The U.S. Department of Agriculture recommends a series of conservation practices to help farmers prepare for drought. Some preventative measures include installing an efficient irrigation system that reduces the amount of water lost to evaporation, storing water in ditches along fields, regularly monitoring soil moisture, planting crops that are more drought-resistant, and rotating crops to allow water in the soil to increase.
     
    In urban areas, many cities are promoting water conservation by addressing water usage habits. Some enforce water restrictions, such as banning car-washing at home, limiting days when lawns and plants can be watered, and offering rebates and assistance programs to fix household leaks. 
     
    Some drought-ravaged cities are taking even more extreme measures to prepare for future droughts. In Australia, the city of Perth is planning to start a massive wastewater-recycling program in 2016 that will eventually provide one-quarter of the city’s water demands. Perth has been dealing with a decline in rainfall since the mid 1970s. The city, which is on the edge of a huge desert, is also struggling with its history of over-consumption of water. Water-hungry traditions such as planting large, lush lawns and parks will need to be addressed through conservation measures.   
  • Term Part of Speech Definition Encyclopedic Entry
    academic Adjective

    person or thing having to do with school, particularly college or university education.

    agriculture Noun

    the art and science of cultivating the land for growing crops (farming) or raising livestock (ranching).

    Encyclopedic Entry: agriculture
    Ancestral Puebloans Plural Noun

    (1200 BCE-1300 CE) people and culture native to what is now the southwestern United States. Also called Anasazi.

    arable Adjective

    land able to produce crops.

    artifact Noun

    material remains of a culture, such as tools, clothing, or food.

    atmospheric circulation Noun

    large-scale movement of air that helps distribute thermal energy (heat) on the surface of the Earth.

    biodiversity Noun

    all the different kinds of living organisms within a given area.

    Encyclopedic Entry: biodiversity
    climate Noun

    all weather conditions for a given location over a period of time.

    Encyclopedic Entry: climate
    climate change Noun

    gradual changes in all the interconnected weather elements on our planet.

    Encyclopedic Entry: climate change
    compact Verb

    to pack tightly together.

    complex Adjective

    complicated.

    conflict Noun

    a disagreement or fight, usually over ideas or procedures.

    conservation Noun

    management of a natural resource to prevent exploitation, destruction, or neglect.

    Encyclopedic Entry: conservation
    Corn Belt Noun

    region whose economy is dominated by the agricultural production of corn. In North America, the Corn Belt sits between the Ohio and Missouri Rivers.

    crop Noun

    agricultural produce.

    Encyclopedic Entry: crop
    customize Verb

    to change or modify an object to a unique set of preferences.

    dam Noun

    structure built across a river or other waterway to control the flow of water.

    data Plural Noun

    (singular: datum) information collected during a scientific study.

    deforestation Noun

    destruction or removal of forests and their undergrowth.

    dehydration Noun

    illness in which the body loses too much water.

    desert Noun

    area of land that receives no more than 25 centimeters (10 inches) of precipitation a year.

    Encyclopedic Entry: desert
    desertification Noun

    the spread of desert conditions in arid regions, usually caused by human activity.

    developing world Noun

    nations with low per-capita income, little infrastructure, and a small middle class.

    disaster area Noun

    region that has been physically and economically damaged by a natural, technological, or social hazard.

    disrupt Verb

    to interrupt.

    drastic Adjective

    severe or extreme.

    drought Noun

    period of greatly reduced precipitation.

    Encyclopedic Entry: drought
    dust Noun

    tiny, dry particles of material solid enough for wind to carry.

    Encyclopedic Entry: dust
    Dust Bowl Noun

    (1930-1940) term for the Great Plains of the U.S. and Canada when severe dust storms forced thousands of people off their farms.

    earthquake Noun

    the sudden shaking of Earth's crust caused by the release of energy along fault lines or from volcanic activity.

    economic Adjective

    having to do with money.

    ecosystem Noun

    community and interactions of living and nonliving things in an area.

    Encyclopedic Entry: ecosystem
    efficient Adjective

    performing a task with skill and minimal waste.

    El Nino Noun

    irregular, recurring weather system that features a warm, eastern-flowing ocean current in the eastern Pacific Ocean.

    Encyclopedic Entry: El Niño
    erosion Noun

    act in which earth is worn away, often by water, wind, or ice.

    Encyclopedic Entry: erosion
    evaporation Noun

    process by which liquid water becomes water vapor.

    Encyclopedic Entry: evaporation
    famine Noun

    an extreme shortage of food in one area during a long period of time.

    farmer Noun

    person who cultivates land and raises crops.

    feature Noun

    non-portable archaeological remains, such as pyramids or post-holes.

    federal Adjective

    having to do with a nation's government (as opposed to local or regional government).

    Federal Emergency Management Agency (FEMA) Noun

    U.S. Homeland Security agency responsible for coordinating response and aid distribution after natural and manmade disasters.

    fertile Adjective

    able to produce crops or sustain agriculture.

    flood Noun

    overflow of a body of water onto land.

    Encyclopedic Entry: flood
    forced migration Noun

    the movement of people away from their homes due to political conflict, natural disaster or environmental hazard.

    forecast Verb

    to predict, especially the weather.

    forest Noun

    ecosystem filled with trees and underbrush.

    frequent Adjective

    often.

    global warming Noun

    increase in the average temperature of the Earth's air and oceans.

    Encyclopedic Entry: global warming
    graze Verb

    to feed on grass, usually over a wide pasture.

    Great Depression Noun

    (1929-1941) period of very low economic activity in the U.S. and throughout the world.

    Great Plains Noun

    grassland region of North America, between the Rocky Mountains and the Mississippi River.

    habitat Noun

    environment where an organism lives throughout the year or for shorter periods of time.

    Encyclopedic Entry: habitat
    hindsight Noun

    recognition of the importance, significant features, or realities of a situation after it has occurred.

    Horn of Africa Noun

    large peninsula in northeast Africa, including the countries of Somalia, Djibouti, Eritrea, and Ethiopia. Also called the Somali Peninsula.

    hurricane Noun

    tropical storm with wind speeds of at least 119 kilometers (74 miles) per hour. Hurricanes are the same thing as typhoons, but usually located in the Atlantic Ocean region.

    ice core Noun

    sample of ice taken to demonstrate changes in climate over many years.

    ignite Verb

    to set on fire.

    inadequate Adjective

    not enough or not of high-enough quality.

    inevitable Adjective

    certain to happen, unavoidable.

    irrigation Noun

    watering land, usually for agriculture, by artificial means.

    Encyclopedic Entry: irrigation
    landscape Noun

    the geographic features of a region.

    Encyclopedic Entry: landscape
    lightning Noun

    sudden electrical discharge from clouds.

    Encyclopedic Entry: lightning
    livestock noun, plural noun

    animals raised for sale and profit.

    logging Noun

    industry engaged in cutting down trees and moving the wood to sawmills.

    Middle East Noun

    region of southwest Asia and northeast Africa.

    minimize Verb

    to make smaller.

    MIssissippian Adjective

    (800-1500) having to do with a network of Native American cultures indigenous to the Mississippi Valley.

    monitor Verb

    to observe and record behavior or data.

    National Weather Service Noun

    branch of the National Oceanic and Atmospheric Association (NOAA) whose mission is to provide "weather, hydrologic, and climate forecasts and warnings for the United States, its territories, adjacent waters and ocean areas, for the protection of life and property and the enhancement of the national economy."

    natural hazard Noun

    event in the physical environment that is destructive to human activity.

    nutrition Noun

    process by which living organisms obtain food or nutrients, and use it for growth.

    onset Noun

    beginning or start of something.

    overgrazing Noun

    process of too many animals feeding on one area of pasture or grassland.

    paleoclimatology Noun

    study of the atmosphere of prehistoric Earth.

    phenomenon Noun

    an unusual act or occurrence.

    poverty Noun

    status of having very little money or material goods.

    precipitation Noun

    all forms in which water falls to Earth from the atmosphere.

    Encyclopedic Entry: precipitation
    prune Verb

    to cut or trim branches from a tree, bush, or shrub.

    rain gauge Noun

    device for measuring rain or other forms of liquid precipitation, usually in millimeters. Also called a precipitation gauge, udometer, pluviometer, or ombrometer.

    resource Noun

    available supply of materials, goods, or services. Resources can be natural or human.

    root system Noun

    all of a plant's roots.

    runoff Noun

    overflow of fluid from a farm or industrial factory.

    Encyclopedic Entry: runoff
    Sahel Noun

    transition zone in northern Africa between the Sahara Desert in the north and the savanna ecosystems in the south.

    sand Noun

    small, loose grains of disintegrated rocks.

    sediment Noun

    underwater soil.

    severe Adjective

    harsh.

    significant Adjective

    important or impressive.

    soil Noun

    top layer of the Earth's surface where plants can grow.

    stall Verb

    to cause to slow or come to a stop.

    storm Noun

    severe weather indicating a disturbed state of the atmosphere resulting from uplifted air.

    supplement Verb

    to increase or add to.

    sustainable Adjective

    able to be continued at the same rate for a long period of time.

    synthesize Verb

    to create or manufacture.

    thermometer Noun

    device that measures temperature.

    Encyclopedic Entry: thermometer
    thunderstorm Noun

    cloud that produces thunder and lightning, often accompanied by heavy rains.

    tornado Noun

    a violently rotating column of air that forms at the bottom of a cloud and touches the ground.

    tree ring Noun

    layered formation in the trunk of a tree that marks its growth at least once a year.

    unemployment Noun

    state of not having a job.

    urban area Noun

    developed, densely populated area where most inhabitants have nonagricultural jobs.

    Encyclopedic Entry: urban area
    vegetation Noun

    all the plant life of a specific place.

    vulnerable Adjective

    capable of being hurt.

    war Noun

    large-scale armed conflict.

    wastewater Noun

    water that has been used for washing, flushing, or industry.

    water cycle Noun

    movement of water between atmosphere, land, and ocean.

    Encyclopedic Entry: water cycle
    water shortage Noun

    reduction in the amount of fresh water available for drinking, hygiene, and industrial and agricultural use.

    weather Noun

    state of the atmosphere, including temperature, atmospheric pressure, wind, humidity, precipitation, and cloudiness.

    Encyclopedic Entry: weather
    wildfire Noun

    uncontrolled fire that happens in a rural or sparsely populated area.

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