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A drought is defined as an extended period of abnormally dry weather that causes water shortages and crop damage. A drought starts when total rainfall is well below average for several months. Other signs of drought include: unusually low river flows, low groundwater and reservoir levels, very dry soil, reduced crop yields or even crop failure, and algae blooms in reservoirs and lakes. Groundwater is not replenished because not enough rain is falling to wet the soil's entire surface area and to be absorbed properly.
Drought conditions lead to increased growth of algae in lakes, ponds and other slow-moving bodies of water. The water is no longer a safe place for fish and other aquatic life. Animals that drink from the rivers or streams can become sick and die; swimmers in affected waters may become ill. The ecology of an area may be affected by the drying of wetlands, with wading birds dying out. Crop production will be lower than usual; trees may die. Wildfires spring up; lack of irrigation can lead to famine and disease.
Sociological consequences of drought range from social unrest to relocation of populations to war.
Some ways to save water:
In the house:
Out of doors:
There have been a number of life-threatening droughts over the centuries. Cape Verde has suffered a number of droughts, and continues to suffer from erratic rainfall. Over 10,000 people starved to death due to droughts in the 1700s and 1800s, and a great many residents migrated to other areas.
In the early 1900s, drought led to the deaths of about 3 million people in India and 5 to 10 million people in the Soviet Union. In China, approximately 3 million people died from famine caused by drought in 1936.
America's "Dust Bowl" was a series of three droughts in the 1930s that forced the migration of large populations in the American Great Plains. Winds whipped up clouds of soil, called "dusters" or "black blizzards," crops were ruined and inhabitants suffered from dust-related health problems. The drought came on the heels of the Great Depression, battering an already impoverished population. John Steinbeck's The Grapes of Wrath told the story of the "Okies" who had to leave their homes and move to California.
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also drouth (drouth)[Middle English, from Old English drūgoth, akin to drȳge, dry.]
droughty drought'y adj.For more information on drought, visit Britannica.com.
A general term implying a deficiency of precipitation of sufficient magnitude to interfere with some phase of the economy. Agricultural drought, occurring when crops are threatened by lack of rain, is the most common. Hydrologic drought, when reservoirs are depleted, is another common form. The Palmer index is used by agriculturalists to express the intensity of drought as a function of rainfall and hydrologic variables.
The meteorological causes of drought are usually associated with slow, prevailing, subsiding motions of air masses from continental source regions. These descending air motions, of the order of 660–1000 ft (200 or 300 m) per day, result in compressional warming of the air and therefore reduction in the relative humidity. Since the air usually starts out dry, and the relative humidity declines as the air descends, cloud formation is inhibited—or if clouds are formed, they are soon dissipated.
Definition: dryness; shortage of supply
Antonyms: monsoon, wetness
A long, continuous period of dry weather. Major causes of drought in Britain are the persistence of warm anticyclones, and the displacement of mid-latitude depressions by blocking anticyclones. Droughts in Africa, for example in the Sahel in the 1970s or in Zimbabwe in the early 1990s, result from the failure of the inter-tropical convergence zone to move sufficiently far from the equator. See absolute drought.
Bibliography
See C. S. Russell et al., Drought and Water Supply (1970); W. C. Palmer and L. M. Denny, Drought Bibliography (1971); R. V. Garcia and J. Escudero, Drought and Man (1986).
During the drought the crops dried up and blew away.
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A drought is an extended period of months or years when a region notes a deficiency in its water supply whether surface or underground water. Generally, this occurs when a region receives consistently below average precipitation. It can have a substantial impact on the ecosystem and agriculture of the affected region. Although droughts can persist for several years, even a short, intense drought can cause significant damage[1] and harm the local economy.[2]
This global phenomenon has a widespread impact on agriculture. Lengthy periods of drought have long been a key trigger for mass migration and played a key role in a number of ongoing migrations and other humanitarian crises in the Horn of Africa and the Sahel.
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Periods of drought can have significant environmental, agricultural, health, economic and social consequences. The effect varies according to vulnerability. For example, subsistence farmers are more likely to migrate during drought because they do not have alternative food sources. Areas with populations that depend on as a major food source are more vulnerable to drought-triggered famine.
Drought can also reduce water quality, because lower water flows reduce dilution of pollutants and increase contamination of remaining water sources. Common consequences of drought include:
Drought is a normal, recurring feature of the climate in most parts of the world. It is among the earliest documented climatic events, present in the Epic of Gilgamesh and tied to the biblical story of Joseph's arrival in and the later Exodus from Ancient Egypt.[9] Hunter-gatherer migrations in 9,500 BC Chile have been linked to the phenomenon,[10] as has the exodus of early humans out of Africa and into the rest of the world around 135,000 years ago.[11]
Modern peoples can effectively mitigate much of the impact of drought through irrigation and crop rotation. Failure to develop adequate drought mitigation strategies carries a grave human cost in the modern era, exacerbated by ever-increasing population densities.
Recurring droughts leading to desertification in the Horn of Africa have created grave ecological catastrophes, prompting massive food shortages, still recurring.[14] To the north-west of the Horn, the Darfur conflict in neighboring Sudan, also affecting Chad, was fueled by decades of drought; combination of drought, desertification and overpopulation are among the causes of the Darfur conflict, because the Arab Baggara nomads searching for water have to take their livestock further south, to land mainly occupied by non-Arab farming peoples.[15]
Approximately 2.4 billion people live in the drainage basin of the Himalayan rivers.[16] India, China, Pakistan, Bangladesh, Nepal and Myanmar could experience floods followed by droughts in coming decades. Drought in India affecting the Ganges is of particular concern, as it provides drinking water and agricultural irrigation for more than 500 million people.[17][18][19] The west coast of North America, which gets much of its water from glaciers in mountain ranges such as the Rocky Mountains and Sierra Nevada, also would be affected.[20][21]
In 2005, parts of the Amazon basin experienced the worst drought in 100 years.[22][23] A 23 July 2006 article reported Woods Hole Research Center results showing that the forest in its present form could survive only three years of drought.[24][25] Scientists at the Brazilian National Institute of Amazonian Research argue in the article that this drought response, coupled with the effects of deforestation on regional climate, are pushing the rainforest towards a "tipping point" where it would irreversibly start to die. It concludes that the rainforest is on the brink of being turned into savanna or desert, with catastrophic consequences for the world's climate. According to the WWF, the combination of climate change and deforestation increases the drying effect of dead trees that fuels forest fires.[26]
By far the largest part of Australia is desert or semi-arid lands commonly known as the outback. A 2005 study by Australian and American researchers investigated the desertification of the interior, and suggested that one explanation was related to human settlers who arrived about 50,000 years ago. Regular burning by these settlers could have prevented monsoons from reaching interior Australia.[27] In June 2008 it became known that an expert panel had warned of long term, maybe irreversible, severe ecological damage for the whole Murray-Darling basin if it does not receive sufficient water by October.[28] Australia could experience more severe droughts and they could become more frequent in the future, a government-commissioned report said on July 6, 2008.[29] Australian environmentalist Tim Flannery, predicted that unless it made drastic changes, Perth in Western Australia could become the world’s first ghost metropolis, an abandoned city with no more water to sustain its population.[30]
East Africa currently faces its worst drought in decades,[31][32] with crops and livestock destroyed.[33] The U.N. World Food Programme recently said that nearly four million Kenyans urgently needed food.[34]
Generally, rainfall is related to the amount of water vapour in the atmosphere, combined with the upward forcing of the air mass containing that water vapour. If either of these are reduced, the result is a drought. This can be triggered by an above average prevalence of high pressure systems, winds carrying continental, rather than oceanic air masses (i.e. reduced water content), and ridges of high pressure areas form with behaviors which prevent or restrict the developing of thunderstorm activity or rainfall over one certain region. Oceanic and atmospheric weather cycles such as the El Niño-Southern Oscillation (ENSO) make drought a regular recurring feature of the Americas along the Midwest and Australia. Guns, Germs, and Steel author Jared Diamond sees the stark impact of the multi-year ENSO cycles on Australian weather patterns as a key reason that Australian aborigines remained a hunter-gatherer society rather than adopting agriculture.[35] Another climate oscillation known as the North Atlantic Oscillation has been tied to droughts in northeast Spain.[36]
Human activity can directly trigger exacerbating factors such as over farming, excessive irrigation,[37] deforestation, and erosion adversely impact the ability of the land to capture and hold water.[38] While these tend to be relatively isolated in their scope, activities resulting in global climate change are expected to trigger droughts with a substantial impact on agriculture[39] throughout the world, and especially in developing nations.[40][41][42] Overall, global warming will result in increased world rainfall.[43] Along with drought in some areas, flooding and erosion will increase in others. Paradoxically, some proposed solutions to global warming that focus on more active techniques, solar radiation management through the use of a space sunshade for one, may also carry with them increased chances of drought.[44]
As a drought persists, the conditions surrounding it gradually worsen and its impact on the local population gradually increases. People tend to define droughts in three main ways:[45]
Strategies for drought protection, mitigation or relief include:
Regional:
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This entry is from Wikipedia, the leading user-contributed encyclopedia. It may not have been reviewed by professional editors (see full disclaimer)
Dansk (Danish)
n. - tørke, nød, tørst, tørhed
Nederlands (Dutch)
droogte, langdurig gebrek, dorst
Français (French)
n. - sécheresse
Deutsch (German)
n. - Dürre, Trockenheit, Mangel
Ελληνική (Greek)
n. - (μετεωρ.) ανομβρία, ξηρασία, αναβροχιά, λειψυδρία
Português (Portuguese)
n. - seca (f)
中文(简体)(Chinese (Simplified))
干旱, 缺乏
中文(繁體)(Chinese (Traditional))
n. - 乾旱, 缺乏
日本語 (Japanese)
n. - 干魃, 長期の欠乏, 欠乏
العربيه (Arabic)
(الاسم) جفاف, قحط
עברית (Hebrew)
n. - בצורת, יובש
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