分析西风带和环流的位置和强度及其对阿古拉斯泄漏和南本格拉上升流的影响

N. Tim, E. Zorita, K. Emeis, F. Schwarzkopf, A. Biastoch, B. Hünicke
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引用次数: 5

摘要

摘要南大西洋和印度洋上的西风带和信风是南部非洲周围区域海洋学的重要驱动因素,包括阿古拉斯流、阿古拉斯泄漏和本格拉上升流等特征。阿古拉斯泄漏构成了从印度洋到南大西洋的暖水和盐水运输的一小部分。在西风带增强时泄漏更强。本文分析了过去2000年、近几十年和21世纪不同观测和模拟大气数据集的风应力与东南风和西风带强度和位置的关系。分析表明,两种风系统的变化是密切相关的,近几十年来,西风带和环流向极地移动,西风带增强。此外,当贸易向极地转移时,南本格拉的上升流略有加强。对21世纪西风带强度和位置的预估取决于假定的二氧化碳排放量及其相对于臭氧强迫的影响。在最强排放情景(RCP8.5)中,模拟结果显示进一步向南移动,而在最弱排放情景(RCP2.6)中,模拟结果显示向北移动,这可能是由于臭氧恢复的影响主导了人为温室强迫的影响。我们的结论是,在过去的几十年里,阿古拉斯的泄漏加剧了,如果不减少温室气体排放,预计泄漏会增加。这将对本格拉的上升流强度产生很小的影响,并可能对上升流区域的水团特征产生影响。阿古拉斯水对上升流水团的贡献增加,将向上升流区域输入更多的预成型营养物质和氧气。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Analysis of the position and strength of westerlies and trades with implications for Agulhas leakage and South Benguela upwelling
Abstract. The westerlies and trade winds over the South Atlantic and Indian Ocean are important drivers of the regional oceanography around southern Africa, including features such as the Agulhas Current, the Agulhas leakage, and the Benguela upwelling. Agulhas leakage constitutes a fraction of warm and saline water transport from the Indian Ocean into the South Atlantic. The leakage is stronger during intensified westerlies. Here, we analyze the wind stress of different observational and modeled atmospheric data sets (covering the last 2 millennia, the recent decades, and the 21st century) with regard to the intensity and position of the southeasterly trades and the westerlies. The analysis reveals that variations of both wind systems go hand in hand and that a poleward shift of the westerlies and trades and an intensification of westerlies took place during the recent decades. Furthermore, upwelling in South Benguela is slightly intensified when trades are shifted poleward. Projections for strength and position of the westerlies in the 21st century depend on assumed CO2 emissions and on their effect relative to the ozone forcing. In the strongest emission scenario (RCP8.5) the simulations show a further southward displacement, whereas in the weakest emission scenario (RCP2.6) a northward shift is modeled, possibly due to the effect of ozone recovery dominating the effect of anthropogenic greenhouse forcing. We conclude that the Agulhas leakage has intensified during the last decades and is projected to increase if greenhouse gas emissions are not reduced. This will have a small impact on Benguela upwelling strength and may also have consequences for water mass characteristics in the upwelling region. An increased contribution of Agulhas water to the upwelling water masses will import more preformed nutrients and oxygen into the upwelling region.
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