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What are the climatic reasons that affect famine in Africa?
Although the Horn of Africa is close to the equator, most of its land is arid and barren. The tropical monsoon with a lot of water vapor enters from the west coast of Africa, bringing abundant rainfall to north-central Africa and Sudan. Before the monsoon reaches Djibouti and Somalia, most of the water vapor has dissipated, so most countries in East Africa have little rainfall in the monsoon rainy season, and only the western and central parts of Ethiopia and the southernmost part of Eritrea have more rainfall.
In winter, affected by the dry northeast trade wind, most parts of the Horn of Africa are dry and lack of rain, and the rainfall in northern Somalia can reach 500mm only in late autumn. On the east coast, affected by the upwelling of the ocean and the northeast trade wind, the annual precipitation is only 50 mm.
There is little precipitation in most parts of East Africa, but the climate is very hot and the evaporation is huge. The coast of the Red Sea is one of the hottest places in the world. The temperature in July is usually around 465,438+0℃, and the temperature at 65,438+0 can reach 32℃. Take the port city of Berbera in northwest Somalia as an example. The average maximum temperature from June to September afternoon is 38℃.
Because of bad weather conditions and weak infrastructure, agriculture in many African countries basically depends on the weather. If the weather is favorable this year and the harvest is good, the economic growth rate will be higher. If there is a natural disaster in the next year, there will definitely be famine. The probability of drought in southern Africa and eastern Africa is high, and famine often occurs.
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