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・ Daho, Burkina Faso
・ Daho-Doo language
・ Dahoam is Dahoam
・ Dahod
・ Dahod (Lok Sabha constituency)
・ Dahod (Vidhan Sabha constituency)
・ Dahod district
・ Dahoga, Pennsylvania
・ DaHok
・ Dahoma, Florida
・ Dahomey
・ Dahomey Amazons
・ Dahomey and Togo by-election, 1946
・ Dahomey at the 1972 Summer Olympics
・ Dahomey Expedition commemorative medal 1892
Dahomey Gap
・ Dahomey National Wildlife Refuge
・ Dahomeyan Administrative Council election, 1925
・ Dahomeyan Administrative Council election, 1928
・ Dahomeyan Administrative Council election, 1930
・ Dahomeyan Administrative Council election, 1932
・ Dahomeyan Administrative Council election, 1934
・ Dahomeyan Administrative Council election, 1936
・ Dahomeyan constitutional referendum, 1958
・ Dahomeyan constitutional referendum, 1964
・ Dahomeyan constitutional referendum, 1968
・ Dahomeyan Democratic Movement
・ Dahomeyan Democratic Party
・ Dahomeyan Democratic Rally
・ Dahomeyan Democratic Union


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Dahomey Gap : ウィキペディア英語版
Dahomey Gap

In West Africa, the Dahomey Gap refers to the portion of the Guinean forest-savanna mosaic that extends all the way to the coast in Benin, Togo and Ghana, thus separating the forest zone that covers much of the south of the region into two separate parts. The forest region west of the gap is called the Upper Guinean forests or Guinean forest zone, and the portion east of the gap is called the Lower Guinean forests, Lower Guinean-Congolian forests, or Congolian Forest Zone.
The major city in the Gap is Accra. Several other cities, such as Kumasi, exist on the fringe of the Gap.
==Causes of dryness==
The dryness of the Dahomey Gap is unusual, given that it lies surrounded by a very wet monsoon belt on all sides, and no mountains block moisture. Yet, Accra in the heart of the Gap receives only 720 millimetres (28 inches) of rainfall per year — less than half the amount needed to sustain tropical rainforest (which would be expected at a latitude of 6° N).
The cause of the dryness of the Dahomey Gap can simply be explained thus:
* In northern winter, high pressure centred on the Sahara sends dry northeasterly trade winds over West Africa, creating a general dry season, including over the Gap.
* In northern summer, an enormous low pressure system known as the ''monsoon'' forms over the huge Africa-Asia-Europe landmass. Centred over approximately Rajasthan and prevented by the huge barrier of the Himalayas from moving further west, it extends a strong trough over West Africa. This trough sends warm and saturated westerly winds over West Africa, creating a wet season peaking in June on the coast (as the trough moves north) and in August inland.
* The coast in the region of the highest rainfall (Guinea, Sierra Leone, Liberia) slopes from southeast to northwest. This aspect means that the moist westerlies are forced to shed enormous quantities of moisture, allowing rainforest to thrive despite a distinct dry season.
* In the Dahomey Gap, however, the coast slopes in such a way (northeast to southwest) that the rain-bearing westerlies flow parallel to the coast. This means they are not forced to give up nearly so much moisture, and thus the climate is much drier, with only a brief rainy season in May and June. Consequently, an open savanna prevails adapted to the moderate rainfall and high evaporation in the hot temperatures.

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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