摘要
Arctic sea ice plays an essential role in regional and global climate by dynamic processes and feedbacks associated with its high reflectivity, thermal insulation especially in presence of snow cover, and brine rejection [1]. Both observations and model simulations show that Arctic sea ice extent has dramatically declined and thinned in the past few decades [2] in response to global warming and cumulative anthropogenic greenhouse gas(GHG)emissions [3,4].
作者
陈卓奇
王绍银
叶玉芳
刘骥平
Georg Heygster
Mohammed Shokr
惠凤鸣
程晓
Zhuoqi Chen;Shaoyin Wang;Yufang Ye;Jiping Liu;Georg Heygster;Mohammed Shokr;Fengming Hui;Xiao Cheng(School of Geospatial Engineering and Science,Sun Yat-sen University,Zhuhai 519000,China;Southern Marine Science and Engineering Guangdong Laboratory(Zhuhai),Zhuhai 519000,China;Department of Atmospheric and Environmental Sciences,State University of New York at Albany,Albany,NY 12222,USA;GEORG-Lab(Geophysical Remote Sensing Lab),Bremen 28359,Germany;Science and Technology Branch,Environment and Climate Change Canada,Toronto ON M3H 5T4,Canada;University Corporation for Polar Research,Zhuhai 519000,China)
基金
supported by the National Key Research and Development Program of China(2019YFC1509104)
the National Natural Science Fundation of China for Distinguished Young Scholars(41925027)。
