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作 者:Hai Xu Yunping Song Yonaton Goldsmith Yunchao Lang
机构地区:[1]Institute of Surface-Earth System Science,Tianjin University,Tianjin 300072,China [2]Institute of Earth Sciences,the Hebrew University of Jerusalem,Jerusalem 91904,Israel [3]Tianjin Key Laboratory of Earth Critical Zone Science and Sustainable Development in Bohai Rim,Tianjin University,Tianjin 300072,China
出 处:《Science Bulletin》2019年第23期1737-1739,共3页科学通报(英文版)
基 金:supported by the joint project between the National Natural Science Foundation of China (41761144070);the Israel Science Foundation (2487/17);the National Natural Science Foundation of China (41672169)
摘 要:The temperature gradient between the northern and southern hemispheres and its influence on the global atmospheric circulations are frontier topics in international climate/paleoclimate studies.Over the past approximately two decades,an important hypothesis in the field of global climate change is that the changes of the Atlantic meridional overturning circulation lead to changes in the temperature gradients between the northern and southern hemisp heres,which affect the mean zonal locations of the Intertropical Convergence Zone(ITCZ)。
关 键 词:TROPICAL RAINFALL CIRCULATION
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