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    Connecting Changing Ocean Circulation with Changing Climate 

    Source: Journal of Climate:;2012:;volume( 026 ):;issue: 007:;page 2268
    Author(s): Winton, Michael; Griffies, Stephen M.; Samuels, Bonita L.; Sarmiento, Jorge L.; Frölicher, Thomas L.
    Publisher: American Meteorological Society
    Abstract: he influence of changing ocean currents on climate change is evaluated by comparing an earth system model?s response to increased CO2 with and without an ocean circulation response. Inhibiting the ocean circulation response, ...
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    Dominance of the Southern Ocean in Anthropogenic Carbon and Heat Uptake in CMIP5 Models 

    Source: Journal of Climate:;2014:;volume( 028 ):;issue: 002:;page 862
    Author(s): Frölicher, Thomas L.; Sarmiento, Jorge L.; Paynter, David J.; Dunne, John P.; Krasting, John P.; Winton, Michael
    Publisher: American Meteorological Society
    Abstract: he authors assess the uptake, transport, and storage of oceanic anthropogenic carbon and heat over the period 1861?2005 in a new set of coupled carbon?climate Earth system models conducted for the fifth phase of the Coupled ...
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    CORRIGENDUM 

    Source: Journal of Climate:;2011:;volume( 024 ):;issue: 019:;page 5195
    Author(s): Roy, Tilla; Bopp, Laurent; Gehlen, Marion; Schneider, Birgit; Cadule, Patricia; Frölicher, Thomas L.; Segschneider, Joachim; Tjiputra, Jerry; Heinze, Christoph; Joos, Fortunat
    Publisher: American Meteorological Society
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    Regional Impacts of Climate Change and Atmospheric CO2 on Future Ocean Carbon Uptake: A Multimodel Linear Feedback Analysis 

    Source: Journal of Climate:;2011:;volume( 024 ):;issue: 009:;page 2300
    Author(s): Roy, Tilla; Bopp, Laurent; Gehlen, Marion; Schneider, Birgit; Cadule, Patricia; Frölicher, Thomas L.; Segschneider, Joachim; Tjiputra, Jerry; Heinze, Christoph; Joos, Fortunat
    Publisher: American Meteorological Society
    Abstract: he increase in atmospheric CO2 over this century depends on the evolution of the oceanic air?sea CO2 uptake, which will be driven by the combined response to rising atmospheric CO2 itself and climate change. Here, the ...
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