The Benguela upwelling area
The Benguela upwelling area
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本格拉上升流区
DOI：
10.1016/0079-6611(83)90013-7
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发表时间：
1983
影响因子：
4.1
通讯作者：
L. Hutchings
中科院分区：
文献类型：
--
作者：
G. Nelson;L. Hutchings
上升流是整个南部非洲西海岸海洋环流的一个特征，从最南端的开普角（南纬 34.35 度）到北部安哥拉和纳米布拉边界附近的弗洛角（南纬 18.4 度）。在近岸风的影响下，这种现象间歇性地从开普角沿南部海岸延伸到非洲大陆最南端的厄加勒斯角。该地区地理概况如图l(a、b)所示
UPWELLING is a feature of oceanic circulation along the entire west coast of southern Africa from Cape Point (34.35 S) m the extreme south to Cape Frlo (18.4 S) near the border between Angola and NamIbla in the north. Under the influence of longshore winds, the phenomenon extends intermittently from Cape Point along the southern coast to Cape Agulhas, the most southern point of the African continent. The geography of the area is shown in Fig. l (a, b)