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Geography of Somalia : ウィキペディア英語版
Geography of Somalia

Somalia is a country located in the Horn of Africa. It is bordered by Ethiopia to the west, Djibouti to the northwest, the Gulf of Aden to the north, the Indian Ocean to the east, and Kenya to the southwest. With a land area of 637,657 square kilometers, Somalia's terrain consists mainly of plateaus, plains and highlands. Its coastline is more than 3,300 kilometers in length, the longest of mainland Africa and the Middle East.
In the far north, the rugged east-west ranges of the Ogo Mountains lie at varying distances from the Gulf of Aden coast. Hot conditions prevail year-round, along with periodic monsoon winds and irregular rainfall. Geology suggests the presence of valuable mineral deposits.
==Climate==
Due to Somalia's proximity to the equator, there is not much seasonal variation in its climate. However, there are some very unpredictable rainfalls that occur sometimes. Hot conditions prevail year-round along with monsoon (periodic seasonal reversing wind accompanied by corresponding changes in precipitation) winds and irregular rainfall. Mean daily maximum temperatures range from , except at higher elevations and along the eastern seaboard, where the effects of a cold offshore current can be felt. In Mogadishu, for instance, average afternoon highs range from to in April. Some of the highest mean annual temperatures in the world have been recorded in the country; Berbera on the northwestern coast has an afternoon high that averages more than from June through September. Nationally, mean daily minimums usually vary from about .〔Hadden, Robert Lee. 2007. ("The Geology of Somalia: A Selected Bibliography of Somalian Geology, Geography and Earth Science." ) Engineer Research and Development Laboratories, Topographic Engineering Center〕 The greatest range in climate occurs in northern Somalia, where temperatures sometimes surpass in July on the littoral plains and drop below the freezing point during December in the highlands.〔 In this region, relative humidity ranges from about 40 percent in the mid-afternoon to 85 percent at night, changing somewhat according to the season.〔
Unlike the climates of most other countries at this latitude, conditions in Somalia range from arid in the northeastern and central regions to semiarid in the northwest and south. In the northeast, annual rainfall is less than ; in the central plateaus, it is about . The northwestern and southwestern parts of the nation, however, receive considerably more rain, with an average of falling per year. Although the coastal regions are hot and humid throughout the year, the hinterland is typically dry and hot.〔
Most of the country receives less than of rain annually, and a large area encompassing the northeast and much of northern Somalia receives as little as . Certain higher areas in the north, however, record more than a year, as do some coastal sites. The southwest receives . Generally, rainfall takes the form of showers or localized torrential rains and is extremely variable. Mean daily maximum temperatures throughout the country range from , except at higher elevations and along the Indian Ocean coast. Mean daily minimum temperatures vary from to more than . Northern Somalia experiences the greatest temperature extremes, with readings ranging from below freezing in the highlands in December to more than in July in the coastal plain skirting the Gulf of Aden. The north's relative humidity ranges from about 40 percent in midafternoon to 85 percent at night, varying somewhat with the season. During the colder months, December to February, visibility at higher elevations is often restricted by fog. Temperatures in the south are less extreme, ranging from about . The hottest months are February through April. Coastal readings are usually five to ten degrees cooler than those inland. The coastal zone's relative humidity usually remains about 70 percent even during the dry seasons.
There are four main seasons around which pastoral and agricultural life revolve, and these are dictated by shifts in the wind patterns. From December to March is the ''Jilal'', the harshest dry season of the year. The main rainy season, referred to as the ''Gu'', lasts from April to June. This period is characterized by the southwest monsoons, which rejuvenate the pasture land, especially the central plateau, and briefly transform the desert into lush vegetation. From July to September is the second dry season, the ''Xagaa'' (pronounced "Hagaa"). The ''Dayr'', which is the shortest rainy season, lasts from October to December.〔 The ''tangambili'' periods that intervene between the two monsoons (October–November and March–May) are hot and humid.〔

抄文引用元・出典: フリー百科事典『 ウィキペディア(Wikipedia)
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