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作 者:William J.RANDEL Laura L.PAN Jianchun BIAN
机构地区:[1]National Center for Atmospheric Research [2]Key Laboratory of Middle Atmosphere and Global Environment Observation, Institute of Atmospheric Physics, Chinese Academy of Sciences
出 处:《Advances in Atmospheric Sciences》2016年第9期1096-1098,共3页大气科学进展(英文版)
摘 要:1. Overview The upper troposphere-lower stratosphere (UTLS) of the Asian summer monsoon (ASM) region is characterized by a continental-scale anticyclonic circulation, which is dynami- cally active and coupled to monsoonal convection. The monsoon anticyclone exhibits anomalous chemical and aerosol characteristics, linked to the outflow of deep convection and the large-scale circulation, and strongly influences the global UTLS composition during boreal summer.1. Overview The upper troposphere-lower stratosphere (UTLS) of the Asian summer monsoon (ASM) region is characterized by a continental-scale anticyclonic circulation, which is dynami- cally active and coupled to monsoonal convection. The monsoon anticyclone exhibits anomalous chemical and aerosol characteristics, linked to the outflow of deep convection and the large-scale circulation, and strongly influences the global UTLS composition during boreal summer.
关 键 词:Transport and Chemistry of the UTLS Asian Monsoon Workshop on Dynamics ASM
分 类 号:P425.42[天文地球—大气科学及气象学] O6[理学—化学]
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