大气和海洋科学快报(英文版)2023,Vol.16Issue(6):22-27,6.DOI:10.1016/j.aosl.2023.100353
Causes of the record-low Antarctic sea-ice in austral summer 2022
Causes of the record-low Antarctic sea-ice in austral summer 2022
摘要
Abstract
2022年夏季(2021年12月至2022年2月)南极海冰面积达到历史新低,西南极减少最显著.2021年8~10月南半球环状模接近历史最强和7~9月海洋性大陆附近海温显著增暖是两个关键因素.由于平流层臭氧破纪录减少使得前者维持历史最强或接近最强,导致阿蒙森低压(ASL)加深并向西南移动,有利于海冰减少.后者持续到夏季,有利于拉尼娜的发展,通过激发罗斯贝波列加深ASL.在热力上,臭氧减少导致向下净短波辐射增加,引起西南极增暖.此外,净短波辐射-海温-云形成正反馈,与埃克曼输送一起,放大表面增暖,从而促进海冰融化.关键词
南极海冰/历史新低/历史最强臭氧损耗/南半球环状模/拉尼娜/阿蒙森低压Key words
Antarctic sea-ice/Record low/Unprecedented stratospheric ozone depletion/Southern annular mode/La Niña/Amundsen Sea Low引用本文复制引用
Chao Zhang,Shuanglin Li..Causes of the record-low Antarctic sea-ice in austral summer 2022[J].大气和海洋科学快报(英文版),2023,16(6):22-27,6.基金项目
This work was jointly supported by a Strategic Project of the Chinese Academy of Sciences[grant number XDA19070402],the National Nat-ural Science Foundation of China[grant number 41790473],and the Post-doctoral Innovation Foundation of Hubei Province. ()