RESEARCH ARTICLE The Contributions of Winter Cloud Anomalies 10.1029/2018JD029435 in 2011 to the Summer Sea‐Ice Rebound Key Points: • Wintertime cloud fraction in 2012 in the Antarctic anomalies in 2011 contributed Yunhe Wang1,4,5 , Xiaojun Yuan3 , Haibo Bi1,2,5, Yu Liang1,4,5 , Haijun Huang1,2,4,5, significantly to the summertime 1,2,5 1,2,5 sea‐ice rebound in 2012 in the Zehua Zhang , and Yanxia Liu Antarctic 1 • Less cloud fraction in winter 2011 CAS Key Laboratory of Marine Geology and Environment, Institute of Oceanology, Chinese Academy of Sciences, related to large‐scale atmospheric Qingdao, China, 2Laboratory for Marine Geology, Qingdao National Laboratory for Marine Science and Technolog, circulation resulted in a strong Qingdao, China, 3Lamont‐Doherty Earth Observatory, Columbia University, New York, NY, USA, 4University of Chinese negative surface‐radiation budget Academy of Sciences, Beijing, China, 5Center for Ocean Mega‐Science, Chinese Academy of Sciences, Qingdao, China • Cloud forcing in winter 2011 cooled the surface, promoted more sea‐ice growth, and resulted in more sea‐ice survival in summer 2012 Abstract Unlike the rapid decline of Arctic sea ice in the warming climate, Antarctic sea‐ice extent exhibits a modest positive trend in the period of near four decades. In recent years, the fluctuation in Antarctic sea ice has been strengthened, including a decrease toward the lowest sea‐ice extent in February – ‐ Correspondence to: 2011 for the period of 1978 2016 and a strong rebound in the summer of 2012. The sea ice recovery mainly H. Bi and H. Huang, occurs in the Weddell Sea, Bellingshausen Sea, Amundsen Sea, southern Ross Sea, and the eastern Somov
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