摘要
Antarctica is considered as an important component of the global climate system, not only because of its ability to drive global sea-level rise through ice melting [1], but also because of its stabilizing effect on global atmospheric energy balance/circulation [2].In recent years, Antarctica has experienced rapid climatic changes and frequent climate extremes, such as a rapid decrease in summer sea ice extent since 2016 [3] and the highest air temperature recorded at Esperanza station in the Antarctic Peninsula on 9February 2020 [4]. In this context, climate extremes in Antarctica have received increasing attention recently [4–7].
作者
王赛
丁明虎
刘舸
赵守栋
张文千
李熙晨
陈文
效存德
秦大河
Sai Wang;Minghu Ding;Ge Liu;Shoudong Zhao;Wenqian Zhang;Xichen Li;Wen Chen;Cunde Xiao;Dahe Qin(State Key Laboratory of Severe Weather,Chinese Academy of Meteorological Sciences,Beijing 100081,China;State Key Laboratory of Cryospheric Science,Northwest Institute of Eco-Environment and Resources,Chinese Academy of Sciences,Lanzhou 730000,China;International Center for Climate and Environment Sciences,Institute of Atmospheric Physics,Chinese Academy of Sciences,Beijing 100029,China;Center for Monsoon System Research,Institute of Atmospheric Physics,Chinese Academy of Sciences,Beijing 100029,China;State Key Laboratory of Earth Surface Processes and Resource Ecology,Beijing Normal University,Beijing 100875,China)
基金
supported by the National Natural Science Foundation of China(42122047 and 42105036)
the Basic Research Fund of the Chinese Academy of Meteorological Sciences(2021Y021 and 2021Z006)。
