A low-level jet along the Benguela coast, an integral part of the Benguela current ecosystem

被引:52
|
作者
Nicholson, Sharon E. [1 ]
机构
[1] Florida State Univ, Dept Meteorol, Tallahassee, FL 32306 USA
基金
美国国家科学基金会;
关键词
OCEAN DYNAMICS EXPERIMENT; MARINE BOUNDARY-LAYER; WEST-AFRICAN SAHEL; RAINFALL VARIABILITY; TROPICAL ATLANTIC; CALIFORNIA COAST; WARM EVENTS; SOUTHERN-OSCILLATION; NORTHERN CALIFORNIA; INDIAN-OCEAN;
D O I
10.1007/s10584-009-9678-z
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
The Benguela Current Ecosystem of Southern Africa is the strongest wind-driven coastal upwelling system known. This is one of the most productive ocean areas in the world, extremely rich in fishery resources with a total catch in excess of one million tons per annum. Marine life off the coast relies heavily on the nutrient-rich upwellings of the cold Benguela current. Warming events occur along this coast in association with many El Nios. These tremendously disrupt the coastal ecosystem, reducing productivity and devastating the anchovy and sardine fisheries. This article demonstrates for the first time the existence of a low-level atmospheric jet along the Benguela Coast of the southeastern Atlantic. Blowing parallel to the coast, this jet drives the coastal upwelling system and is part of a mechanism that links Pacific El Nio events to Southern Africa. The existence of such a jet has tremendous implications for the Benguela current and its response to climatic variability and change because a positive feedback exists between the intensity of this jet and the intensity of coastal upwelling. This may enhance the response of the Benguela Current Ecosystem to climatic variability, making it particularly susceptible to the impacts of global climate change.
引用
收藏
页码:613 / 624
页数:12
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