Local processes dominate over remote processes in polar amplification
Malte F Stuecker1, Cecilia M Bitz2, Kyle Armour2, Cristian Proistosescu3, Sarah M Kang4, Shang-Ping Xie5, Doyeon Kim6, Dr. Shayne McGregor7, Wenjun Zhang8, Sen Zhao9, Wenju Cai10, Yue Dong11 and Fei-Fei Jin12, (1)IBS Center for Climate Physics (ICCP), Busan, South Korea, (2)University of Washington, Department of Atmospheric and Climate Science, Seattle, United States, (3)University of Illinois Urbana Champaign, Department of Climate, Meteorology & Atmospheric Sciences, Urbana, United States, (4)Ulsan National Institute of Science and Technology, Ulsan, Germany, (5)University of California San Diego, Scripps Institution of Oceanography, La Jolla, United States, (6)Ulsan National Institute of Science and Technology, Ulsan, South Korea, (7)Monash University, School of Earth, Atmosphere and Environment, Melbourne, VIC, Australia, (8)NUIST Nanjing University of Information Science and Technology, Nanjing, China, (9)IAP Insititute of Atmospheric Physics, Chinese Academy of Sciences, Beijing, China, (10)Laoshan Laboratory, Qingdao, China, (11)University of Washington, Department of Atmospheric Sciences, Seattle, WA, United States, (12)University of Hawaii at Manoa, Department of Atmospheric Sciences and International Pacific Research Center, Honolulu, United States
