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Drought
DICTIONARY DEFINITIONS of drought are very straightforward and brief: drought is a long period without rainfall. There have been many periods of this type, and the impact of a severe drought on people and animals within the affected region has been devastating. There are many examples of the impact of severe drought.
The Dust Bowl in the 1930s forced many thousands of people to abandon their land in the midwest of the United States. Drought in the Sahel region of Africa from 1968 to 1974 took the lives of hundreds of thousands of people and millions of farm animals. In the first few years of the 21st century, the threat of drought is widespread. Large areas in sub-Saharan Africa continue to suffer from lack of rainfall. In southern Africa, estimates suggest that more than 15 million people are at risk of starvation. Ethiopia is another African country in danger of losing millions of people because of drought and ensuing famine. Experts speculate that the loss of life in the current crisis could exceed the 1984 to 1985 drought occurrence when over one million people perished. The Sahel, the semidesert region adjacent to the southern edge of the Sahara, is having food shortages because of low agricultural production during periods of persistent drought. Other regions in the world are also having drought conditions more frequently than in the past. All indications are that this situation will continue in the most susceptible regions.
The explanation for drought is complex. Both natural occurrences and the actions of humans contribute to drought formation. The areas most prone to drought are the semideserts that lie adjacent to the great deserts of the world. Deserts originally formed beneath the naturally occurring high-pressure systems centered at approximately 30 degrees north and south of the equator. These regions are under the influence of dry air descending from the high-pressure systems. The deserts are essentially devoid of vegetation and receive low levels of precipitation. The Atacama Desert in South America is extremely dry: no rainfall has ever been recorded in large parts of this desert.
Desertification and Land Degradation
The largest of the world's great deserts is the Sahara in north Africa. Deserts are found on every major continent, and evidence indicates that the deserts are in fact expanding. In 1977 a United Nations study pointed out that the areas on the margins of the great deserts are becoming drier. In some cases, especially in the Sahel, the Sahara is continually moving south and replacing the semidesert. In a transformation of this type, the vegetative complement of the semidesert, the attribute that identifies it as a distinct climatic type, disappears and the area becomes desert. The term given to the process of increased aridity and the transformation of the semidesert is desertification, and its origins and anticipated expanse are the topic of discussion by development experts worldwide.
There is little doubt that desertification is due in part to climatic change, a process that has been under way on earth for millennia. But climate change is only one of the contributing factors. There is also the strong argument that desertification is to a great extent human-induced. In order for agriculture to take place, the land must be cleared and opened for planting. If sufficient rainfall is present at the right times during the growing season, the system operates in good order. However, exceptionally dry conditions can negatively impact agricultural activity in a number of ways. If it is especially dry at the beginning of the season, planting may have to be delayed. If this is the case, winds can blow away the fertile topsoil and the new seeds if they have been planted. Drought conditions can negatively impact a crop later in the growth cycle; for example, if corn does not receive sufficient rainfall during the last stages of plant maturity, an entire crop can be decimated. Overgrazing can reduce the plant cover in semiarid regions, reducing the amount of plant growth in the following year.
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