supported by the National Key Research and Development Program of China (2018YFA0605700);supported by the Joint Research Centre for Southern Hemisphere Oceans Research (CSHOR)between the Qingdao National Laboratory for Marine Science and Technology (QNLM)and the Commonwealth Scientific and Industrial Research Organisation (CSIRO);supported by the Australian Research Council Special Research Initiative for Securing Antarctica’s Environmental Future (SR200100005);supported by the National Natural Science Foundation of China (41876231);supported by the National Natural Science Foundation of China (42230405 and 41976006);the National Natural Science Foundation of China (41876008 and 41730534);supported by the National Natural Science Foundation of China (41830538);the Program of Impact and Response of Antarctic Seas to Climate Change (IRASCC 01-01-01A);supported by the National Key Research and Development Program of China (2020YFA0608801);the Youth Innovation Promotion Association of Chinese Academy of Sciences (2021205);supported by the National Science Foundation (AGS-1934392);supported by the National Science Foundation (OCE-2048336);the International Partnership Program of Chinese Academy of Sciences (183311KYSB20200015)。
supported by Project of Southern Marine Science and Engineering Guangdong Laboratory(Zhuhai)(SML2021SP312);the National Natural Science Foundation of China(4207506242130601,and 41922044);the National Key Research&Development Program of China(2018YFC1506003);the Fundamental Research Funds for the Central Universities,China(lzujbky-2021ey04);Young Doctoral Funds for Gansu Provincial Education Department(2021QB-009);supported by Supercomputing Center of Lanzhou University。
The Arctic has experienced several extreme springtime stratospheric ozone depletion events over the past four decades,particularly in 1997,2011 and 2020.However,the impact of this stratospheric ozone depletion on the ...