A review of the interaction between the cryosphere and atmosphere

作     者：YongJian Ding JianPing Yang ShengXia Wang YaPing Chang YongJian Ding;JianPing Yang;ShengXia Wang;YaPing Chang

作者机构：State Key Laboratory of Cryospheric ScienceNorthwest Institute of Eco-Environment and ResourcesChinese Academy of SciencesLanzhouGansu 730000China China-Pakistan Joint Research Center on Earth ScienceCAS-HECIslamabadPakistan University of Chinese Academy of SciencesBeijing 100049China 

出 版 物：《Research in Cold and Arid Regions》 (寒旱区科学（英文版）)

年 卷 期：2020年第12卷第6期

页      面：329-342页

核心收录：

学科分类：0830[工学-环境科学与工程（可授工学、理学、农学学位）] 0709[理学-地质学] 07[理学] 0818[工学-地质资源与地质工程] 0708[理学-地球物理学] 0705[理学-地理学] 0815[工学-水利工程] 070501[理学-自然地理学] 0706[理学-大气科学] 0813[工学-建筑学] 0814[工学-土木工程] 

基　　金：This work is supported by the National Natural Science Foundation of China(41730751,41421061) the Strategic Priority Research Program of the Chinese Academy of Sciences,No.XDA23060700.The authors thank two anonymous reviewers for their suggestions leading to significant improvement in the paper.We thank all persons for their help to us. 

主　　题：climate warming cryosphere atmosphere response feedback 

摘      要：The interaction between the cryosphere and atmosphere is an essential and extremely sensitive mutual action process on the earth.Due to global warming and the cryospheric melting,more and more attention has been paid to the interaction process between the cryosphere and atmosphere,especially the feedback of the cryosphere change to the atmosphere.A comprehensive review of the studies on the interaction between the cryosphere and atmosphere is conducted from two aspects:(1)effects of climate change on the cryosphere or responses of the cryosphere to climate change;and(2)feedback of the cryosphere change to the climate.The response of the cryosphere to climate change is lagging.Such a lagging and cumulative effect of temperature rise within the cryosphere have resulted in a rapid change in the cryosphere in the 21st century,and its impacts have become more significant.The feedback from cryosphere change on the climate are omnifarious.Among them,the effects of sea ice loss and snow cover change,especially the Arctic sea ice loss and the Northern Hemisphere snow cover change,are the most prominent.The Arctic amplification(AA)associated with sea ice feedback is disturbing,and the feedback generated by the effect of temperature rise on snow properties in the Northern Hemisphere is also of great concern.There are growing evidence of the impact of the Arctic cryosphere melting on mid-latitude weather and climate.Weakened storm troughs,steered jet stream and amplified planetary waves associated with energy propagation become the key to explaining the links between Arctic cryosphere change and atmospheric circulation.There is still a great deal of uncertainty about how cryosphere change affects the weather and climate through different atmospheric circulation processes at different spatial and temporal scales due to observation and simulation problems.