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    The Climate Sensitivity and Its Components Diagnosed from Earth Radiation Budget Data 

    Source: Journal of Climate:;2006:;volume( 019 ):;issue: 001:;page 39
    Author(s): Forster, Piers Mde F.; Gregory, Jonathan M.
    Publisher: American Meteorological Society
    Abstract: One of the major uncertainties in the ability to predict future climate change, and hence its impacts, is the lack of knowledge of the earth?s climate sensitivity. Here, data are combined from the 1985?96 Earth Radiation ...
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    A Surface Energy Perspective on Climate Change 

    Source: Journal of Climate:;2009:;volume( 022 ):;issue: 010:;page 2557
    Author(s): Andrews, Timothy; Forster, Piers M.; Gregory, Jonathan M.
    Publisher: American Meteorological Society
    Abstract: A surface forcing response framework is developed that enables an understanding of time-dependent climate change from a surface energy perspective. The framework allows the separation of fast responses that are unassociated ...
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    Understanding Land–Sea Warming Contrast in Response to Increasing Greenhouse Gases. Part I: Transient Adjustment 

    Source: Journal of Climate:;2009:;volume( 022 ):;issue: 011:;page 3079
    Author(s): Dong, Buwen; Gregory, Jonathan M.; Sutton, Rowan T.
    Publisher: American Meteorological Society
    Abstract: Climate model simulations consistently show that surface temperature over land increases more rapidly than over sea in response to greenhouse gas forcing. The enhanced warming over land is not simply a transient effect ...
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    The Key Role of the Western Boundary in Linking the AMOC Strength to the North–South Pressure Gradient 

    Source: Journal of Physical Oceanography:;2012:;Volume( 042 ):;issue: 004:;page 628
    Author(s): Sijp, Willem P.; Gregory, Jonathan M.; Tailleux, Remi; Spence, Paul
    Publisher: American Meteorological Society
    Abstract: key idea in the study of the Atlantic meridional overturning circulation (AMOC) is that its strength is proportional to the meridional density gradient or, more precisely, to the strength of the meridional pressure gradient. ...
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    Precise Calculations of the Existence of Multiple AMOC Equilibria in Coupled Climate Models. Part I: Equilibrium States 

    Source: Journal of Climate:;2011:;volume( 025 ):;issue: 001:;page 282
    Author(s): Sijp, Willem P.; England, Matthew H.; Gregory, Jonathan M.
    Publisher: American Meteorological Society
    Abstract: his study examines criteria for the existence of two stable states of the Atlantic Meridional Overturning Circulation (AMOC) using a combination of theory and simulations from a numerical coupled atmosphere?ocean climate ...
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    On the Link between the Two Modes of the Ocean Thermohaline Circulation and the Formation of Global-Scale Water Masses 

    Source: Journal of Climate:;2003:;volume( 016 ):;issue: 017:;page 2797
    Author(s): Saenko, Oleg A.; Weaver, Andrew J.; Gregory, Jonathan M.
    Publisher: American Meteorological Society
    Abstract: A close link between the formation of global-scale water masses, such as North Atlantic Deep Water (NADW) and Antarctic Intermediate Water (AAIW), and two stable modes of the thermohaline circulation (THC) is investigated ...
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    Processes Governing the Recovery of a Perturbed Thermohaline Circulation in HadCM3 

    Source: Journal of Climate:;2002:;volume( 015 ):;issue: 007:;page 764
    Author(s): Vellinga, Michael; Wood, Richard A.; Gregory, Jonathan M.
    Publisher: American Meteorological Society
    Abstract: In an experiment with the latest version of the Hadley Centre climate model the model response has been analyzed after the thermohaline circulation (THC) in the Atlantic Ocean has been suppressed. The suppression is induced ...
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    The Role of Climate Sensitivity and Ocean Heat Uptake on AOGCM Transient Temperature Response 

    Source: Journal of Climate:;2002:;volume( 015 ):;issue: 001:;page 124
    Author(s): Raper, Sarah C. B.; Gregory, Jonathan M.; Stouffer, Ronald J.
    Publisher: American Meteorological Society
    Abstract: The role of climate sensitivity and ocean heat uptake in determining the range of climate model response is investigated in the second phase of the Coupled Model Intercomparison Project (CMIP2) AOGCM results. The fraction ...
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    Impact of Mesoscale Eddy Transfer on Heat Uptake in an Eddy-Parameterizing Ocean Model 

    Source: Journal of Climate:;2018:;volume 031:;issue 020:;page 8589
    Author(s): Saenko, Oleg A.; Yang, Duo; Gregory, Jonathan M.
    Publisher: American Meteorological Society
    Abstract: AbstractUsing a set of experiments with an eddy-parameterizing ocean model, it is found that the strength of the Atlantic meridional overturning circulation (AMOC) intensifies with the decrease of the density-dependent ...
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    The Dependence of Radiative Forcing and Feedback on Evolving Patterns of Surface Temperature Change in Climate Models 

    Source: Journal of Climate:;2014:;volume( 028 ):;issue: 004:;page 1630
    Author(s): Andrews, Timothy; Gregory, Jonathan M.; Webb, Mark J.
    Publisher: American Meteorological Society
    Abstract: xperiments with CO2 instantaneously quadrupled and then held constant are used to show that the relationship between the global-mean net heat input to the climate system and the global-mean surface air temperature change ...
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