Revisiting the wintertime emergent constraint of the southern hemispheric midlatitude jet response to global warming

Philippe Breul, P. Ceppi, T. Shepherd
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引用次数: 1

Abstract

Abstract. Most climate models show a poleward shift of the southern hemispheric zonal-mean jet in response to climate change, but the inter-model spread is large. In an attempt to constrain future jet responses, past studies have identified an emergent constraint between the climatological jet latitude and the future jet shift in austral winter. However, we show that the emergent constraint only arises in the zonal mean and not in separate halves of the hemisphere, which questions the physicality of the emergent constraint. We further find that the zonal-mean jet latitude does not represent the latitude of a zonally coherent structure, due to the presence of a double-jet structure in the Pacific region during this season. The zonal asymmetry causes the previously noted large spread in the zonal-mean climatology but not in the response, which underlies the emergent constraint. We therefore argue that the emergent constraint on the zonal-mean jet cannot narrow down the spread in future wind responses, and we propose that emergent constraints on the jet response in austral winter should be based on regional rather than zonal-mean circulation features.
重新考察南半球中纬度急流对全球变暖响应的冬季紧急约束
摘要大多数气候模式显示南半球纬向平均喷流随气候变化向极地移动,但模式间传播较大。为了限制未来的急流响应,过去的研究已经确定了气候急流纬度和未来南方冬季急流转移之间的紧急约束。然而,我们表明紧急约束只出现在区域平均值中,而不是在半球的单独一半中,这质疑了紧急约束的物理性。我们进一步发现,由于本季太平洋地区存在双射流结构,纬向平均急流纬度并不代表纬向相干结构的纬度。纬向不对称导致了之前提到的纬向平均气候学的大传播,而不是响应的大传播,这是紧急约束的基础。因此,我们认为纬向平均急流的紧急约束不能缩小未来风响应的传播范围,我们建议南方冬季急流响应的紧急约束应基于区域而不是纬向平均环流特征。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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CiteScore
6.40
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