Human Impact on Droughts

Drought is an extended period of exceptionallywriter John Steinbeck in his award-winning novel
low precipitation. A drought can feature additionalThe Grapes of Wrath, many farm families had to
weather characteristics, including highabandon their land.
temperatures and high winds. Although lowDrought and famine have severely affected areas
precipitation (rain, snow, or sleet) marks boththroughout Africa. Beginning in the late 1960s, in
droughts and deserts, the two are different. Athe Sahel region south of the Sahara Desert in
desert is a region that experiences lownorthern Africa, a prolonged drought contributed
precipitation as an everyday occurrence. Ato the deaths of an estimated 100,000 people.
drought, on the other hand, is a temporaryThe region was struck again by drought in the
condition in which precipitation is abnormally lowmid-1980s and early 1990s. War and drought in
for a particular region. Droughts may occur at anyEthiopia in the early 1980s brought about the
time in any part of the world and last anywherestarvation of an estimate one million people and
from days to weeks to decades.the forced migration of hundreds of thousands of
The U.S. National Weather Service recognizesothers. Drought combined with social unrest
three categories of drought. A dry spell occurscontinued to afflict many countries at the
when there is less than .08 centimeter (.03 inch)beginning of the twenty-first century. The African
of rainfall during a minimum of 15 consecutivenations of Djibouti, Eritrea, Ethiopia, Kenya,
days. A partial drought occurs when the averageSomalia, and Sudan were all hit hard by a massive
daily rainfall does not exceed .02 centimeter (.008drought that began in the late 1990s. Conflicts like
inch) during a 29-day period. An absolute droughtthe border war between Eritrea and Ethiopia
occurs when there is no measurable rainfall over aslowed the delivery of famine aid. Devastating civil
period of at least 15 days. The intensity of awars also worsened the effect of drought in the
drought may be measured by the ability of livingcountries of Afghanistan and Tajikistan. The
things in the affected area to tolerate the dryunrelenting droughts were the worst those
conditions. Some plants quickly fall prey tocountries had seen in decades.
droughts while others, such as cacti and mesquiteThe El Niño weather phenomenon typically
trees, survive dry conditions by either storingbrings about droughts in various parts of the
water in their tissues or by going dormant (aworld as it disrupts normal weather patterns.
state in which growth activity stops). Although aPerhaps one of the worst such droughts occurred
drought may end abruptly with the return ofin Southeast Asia as a result of the 1997–98
adequate rainfall, the effects of a drought on theEl Niño period. The monsoon rains that normally
landscape and its inhabitants may last for years.drench the area each September were delayed.
Droughts have taken place around the worldConsequently, the jungle fires set by farmers to
throughout history. Some scientists theorize thatclear land were not damped by the usual rain, but
droughts brought about the migrations of earlyinstead raged out of control, propelled by hot
humans. From 1876 to 1879, severe droughts inwinds. The smoke from the fires hung over
China caused the deaths of millions of peopleSoutheast Asia like a thick, dirty blanket. It quickly
from lack of food. In 1921, a drought along thebecame the worst pollution crisis in world history.
Volga River basin in Russia led to the deaths ofAt least 1,000 people died from breathing the
almost five million people, more than the totaltoxic air; several hundred thousand more were
number of deaths in World War I (1914–18).sickened.
The best-known American drought occurred onSoil that lacks humus (nutrient-rich material
the Great Plains region during the mid-1930s.resulting from decaying plants) and the binding
Labeled the Dust Bowl, the affected areaproperty of plant roots cannot absorb or retain
covered almost 50 million acres in parts ofmoisture properly. Dry, crusty soil is easily moved
Colorado, New Mexico, Kansas, Texas, andby winds. The overgrazing of farm animals, the
Oklahoma. During this period, dust stormsover cultivation of farmland, and the clear-cutting
destroyed crops and buried agricultural fields withof forests all contribute to such soil conditions,
drifting sand and dust. As depicted by Americanadding to the severity of droughts.