人为温室气体和气溶胶引发的不同海洋热浪

Xianglin Ren, Wei Liu, Robert J. Allen, Se-Yong Song
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引用次数: 0

摘要

在气候变化不断升级的时代,了解人类对海洋热浪的影响变得至关重要。本研究利用气候模式的历史模拟和单一强迫模拟,深入研究了过去几十年来人为温室气体和气溶胶在塑造全球大暖风特征方面的个别作用。结果表明,温室气体的变化导致了持续时间更长、频率更高和强度更大的热浪。相比之下,人为气溶胶则显著地抑制了强热带气旋的强度和增长。对海表温度概率分布的进一步分析表明,人为温室气体和气溶胶对海表温度概率分布尾部的影响相反,分别导致海表温度尾部扩张和收缩。极端气候(如mhw)因此得到促进和减少。我们的研究强调了人为温室气体和气溶胶对高强度海温的显著影响,这远远超出了这些人为强迫通过改变平均状态海温而改变全球海温概率来调节极端气候的习惯概念。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Distinct anthropogenic greenhouse gas and aerosol induced marine heatwaves
In the era of escalating climate change, understanding human impacts on marine heatwaves (MHWs) becomes essential. This study harnesses climate model historical and single forcing simulations to delve into the individual roles of anthropogenic greenhouse gases and aerosols in shaping the characteristics of global MHWs over the past several decades. The results suggest that greenhouse gas variations lead to longer-lasting, more frequent, and intense MHWs. In contrast, anthropogenic aerosols markedly curbs the intensity and growth of MHWs. Further analysis of the sea surface temperature (SST) probability distribution reveals that anthropogenic greenhouse gases and aerosols have opposing effects on the tails of the SST probability distribution, causing the tails to expand and contract, respectively. Climate extremes such as MHWs are accordingly promoted and reduced. Our study underscores the significant impacts of anthropogenic greenhouse gases and aerosols on MHWs, which go far beyond the customary concept that these anthropogenic forcings modulate climate extremes by shifting global SST probabilities via modifying the mean-state SST.
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