中非东部风和海温的现在和未来趋势

M. García‐Reyes, S. Mahongo
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引用次数: 1

摘要

就气候而言,中非东部海岸是一个充满活力的地区,渔业和与海洋有关的服务影响着很大一部分人口。区域动态的主要驱动力是东北季风和东南季风的季节交替。与这些季风相关的风调节了普遍存在的、受远程影响的东非海岸流(EACC)。本文利用再分析和重建资料,以及综合环流模式,研究了东太平洋和邻近地区的风和海温(SST)的现在和未来趋势。风和海温呈单向变化趋势,东北季风和东南季风在量级和空间上存在差异。索马里地区过去和未来的东北季候风呈现减弱趋势;东南季候风无明显趋势。整个区域海温在过去和未来均呈上升趋势,索马里近海东北季候风增温更强;东洋海温趋势较小。这些趋势可能通过增加水柱稳定性和减少上升流来影响东太平洋,这是由于东太平洋与大陆分离的转移。然而,考虑到分析数据的粗糙分辨率,区域建模仍然是必要的,以了解对东部地区局部动态和生产力的影响。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Present and future trends in winds and SST off central East Africa
The coast of central East Africa (CEA) is a dynamic region in terms of climate, in which fisheries and marine-related services impact a large portion of the population. The main driver of regional dynamics is the seasonal alternation of the Northeast (NE) and Southeast (SE) monsoons. Winds associated with these monsoons modulate the prevalent, remotely-forced East African Coastal Current (EACC). Here, present and future trends in winds and sea surface temperature (SST) of the CEA and adjacent regions are investigated using reanalysis and reconstructed data, and an ensemble of General Circulation Models. It was found that the winds and SST show unidirectional trends, with magnitude and spatial differences between the NE and SE monsoons. Winds show weakening trends during the NE monsoon, in the past and future, of the Somali region; with no significant trends during the SE monsoon. SST shows increasing trends in the entire region in the past and future, with stronger warming during the NE monsoon off Somalia; SST trends are smaller in the CEA. These trends could impact the CEA through increased water-column stability and decreased upwelling due to shifting of the EACC separation from the continent. However, given the coarse resolution of data analyzed, regional modeling is still necessary to understand the impacts on local dynamics and productivity in the CEA.
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