Climate
The predominant climate type is tropical monsoon, with wide topographic-induced variation. The Ethiopian Highlands cover most of the country and have a climate which is generally considerably cooler than other regions at similar proximity to the Equator. Most of the country's major cities are located at elevations of around 2,000–2,500 m (6,562–8,202 ft) above sea level, including historic capitals such as Gondar and Axum.
The modern capital, Addis Ababa, is situated on the foothills of Mount Entoto at an elevation of around 2,400 metres (7,900 ft). It experiences a mild climate year round. With temperatures fairly uniform year round, the seasons in Addis Ababa are largely defined by rainfall: a dry season from October to February, a light rainy season from March to May, and a heavy rainy season from June to September. The average annual rainfall is approximately 1,200 millimetres (47 in).
There are on average 7 hours of sunshine per day. The dry season is the sunniest time of the year, though even at the height of the rainy season in July and August there are still usually several hours per day of bright sunshine. The average annual temperature in Addis Ababa is 16 °C (60.8 °F), with daily maximum temperatures averaging 20–25 °C (68.0–77.0 °F) throughout the year, and overnight lows averaging 5–10 °C (41.0–50.0 °F).
Most major cities and tourist sites in Ethiopia lie at a similar elevation to Addis Ababa and have a comparable climate. In less elevated regions, particularly the lower lying Ethiopian xeric grasslands and shrublands in the east of the country, the climate can be significantly hotter and drier. Dallol, in the Danakil Depression in this eastern zone, has the world's highest average annual temperature of 34 °C (93.2 °F).
출처 : Wikipedia
Climate (bega, kremt, belg)
Because Ethiopia is located in the tropical latitudes, its areas of lower elevation experience climatic conditions typical of tropical savanna or desert. However, relief plays a significant role in moderating temperature, so higher elevations experience weather typical of temperate zones. Thus, average annual temperatures in the highlands are in the low 60s F (mid-10s C), while the lowlands average in the low 80s F (upper 20s C).
There are three seasons in Ethiopia. From September to February is the long dry season known as the bega; this is followed by a short rainy season, the belg, in March and April. May is a hot and dry month preceding the long rainy season (kremt) in June, July, and August. The coldest temperatures generally occur in December or January (bega) and the hottest in March, April, or May (belg). However, in many localities July has the coldest temperatures because of the moderating influence of rainfall.
Ethiopia can be divided into four rainfall regimes. Rain falls year-round in the southern portions of the Western Highlands, where annual precipitation may reach 80 inches (2,000 mm). Summer rainfall is received by the Eastern Highlands and by the northern portion of the Western Highlands; annual precipitation there may amount to 55 inches (1,400 mm). The Eastern Lowlands get rain twice a year, in April–May and October–November, with two dry periods in between. Total annual precipitation varies from 20 to 40 inches (500 to 1,000 mm). The driest of all regions is the Denakil Plain, which receives less than 20 inches (500 mm) and sometimes none at all.
출처 : 브리태니카 백과사전
출처 : NASA
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