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Slowing down of the summer Southern Hemisphere Annular Mode trend against the background of ozone recoveryOA

中文摘要

20世纪末期,南半球热带外地区经历了显著的气候变化,包括夏季南半球环状模(SAM)的显著上升趋势,伴随着南极半岛的增暖和别林斯高晋海的海冰融化.这些趋势主要是由20世纪末期南极平流层臭氧消耗所驱动的.本文发现,自2001年左右以来,在南极平流层臭氧恢复的背景下,观测到的夏季SAM的上升趋势已经趋于平缓,验证了前人利用数值模拟预测的夏季SAM上升趋势减缓现象,与SAM在臭氧恢复后趋势只减缓但没有逆转不同,南极地表气温和海冰的趋势发生了逆转.南极半岛由变暖趋势转为降温趋势,别林斯高晋海域的海冰由融化趋势转为增多趋势.

Fei Zheng;

School of Atmospheric Sciences,Key Laboratory of Tropical Atmosphere-Ocean System,Ministry of Education,Sun Yat-sen University,Zhuhai,China Southern Marine Science and Engineering Guangdong Laboratory,Zhuhai,China

地理科学

南半球环状模南极臭氧损耗南极臭氧恢复

《Atmospheric and Oceanic Science Letters》 2024 (001)

P.1-8 / 8

supported by the National Key Research and Development Project[grant number 2020YFA0608902];the Natural Science Foundation of Guangdong Province[grant number 2023A1515010889].

10.1016/j.aosl.2023.100375

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