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    Coupled Ocean–Atmosphere Responses to Recent Freshwater Flux Changes over the Kuroshio–Oyashio Extension Region 

    Source: Journal of Climate:;2010:;volume( 024 ):;issue: 005:;page 1507
    Author(s): Zhang, Liping; Wu, Lixin; Zhang, Jiaxu
    Publisher: American Meteorological Society
    Abstract: Observations have indicated a trend of freshwater loss in the global western boundary current extension regions over several recent decades. In this paper, the coupled ocean?atmosphere response to the observed freshwater ...
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    Simulated Response to Recent Freshwater Flux Change over the Gulf Stream and Its Extension: Coupled Ocean–Atmosphere Adjustment and Atlantic–Pacific Teleconnection 

    Source: Journal of Climate:;2011:;volume( 024 ):;issue: 015:;page 3971
    Author(s): Zhang, Liping; Wu, Lixin; Zhang, Jiaxu
    Publisher: American Meteorological Society
    Abstract: ecent observation has shown that the dominant mode of the net freshwater flux variations over the North Atlantic Ocean is the significant trend of freshwater loss over the Gulf Stream region and its extension. In this ...
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    Coupled Ocean–Atmosphere Response to Idealized Freshwater Forcing over the Western Tropical Pacific 

    Source: Journal of Climate:;2009:;volume( 023 ):;issue: 007:;page 1945
    Author(s): Wu, Lixin; Sun, Yan; Zhang, Jiaxu; Zhang, Liping; Minobe, Shoshiro
    Publisher: American Meteorological Society
    Abstract: The coupled ocean?atmosphere responses to idealized freshwater forcing in the western tropical Pacific are studied using a fully coupled climate model. The model explicitly demonstrates that freshwater forcing in the western ...
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    Global Hydrological Cycle Response to Rapid and Slow Global Warming 

    Source: Journal of Climate:;2013:;volume( 026 ):;issue: 022:;page 8781
    Author(s): Back, Larissa; Russ, Karen; Liu, Zhengyu; Inoue, Kuniaki; Zhang, Jiaxu; Otto-Bliesner, Bette
    Publisher: American Meteorological Society
    Abstract: his study analyzes the response of global water vapor to global warming in a series of fully coupled climate model simulations. The authors find that a roughly 7% K?1 rate of increase of water vapor with global surface ...
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    Can the Salt-Advection Feedback Be Detected in Internal Variability of the Atlantic Meridional Overturning Circulation? 

    Source: Journal of Climate:;2018:;volume 031:;issue 016:;page 6649
    Author(s): Cheng, Wei; Weijer, Wilbert; Kim, Who M.; Danabasoglu, Gokhan; Yeager, Steve G.; Gent, Peter R.; Zhang, Dongxiao; Chiang, John C. H.; Zhang, Jiaxu
    Publisher: American Meteorological Society
    Abstract: AbstractEvidence for the assumptions of the salt-advection feedback in box models is sought by studying the Atlantic meridional overturning circulation (AMOC) internal variability in the long preindustrial control runs of ...
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