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    The Role of Horizontal Boundaries in Parameter Sensitivity and Decadal-Scale Variability of Coarse-Resolution Ocean General Circulation Models 

    Source: Journal of Physical Oceanography:;1996:;Volume( 026 ):;issue: 003:;page 289
    Author(s): Winton, Michael
    Publisher: American Meteorological Society
    Abstract: Coarse-resolution f-plane and ?-plane frictional geostrophic models are used to study the response to restored surface buoyancies and fixed surface buoyancy fluxes. With restored surface buoyancies it is found that the ...
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    The Effect of Cold Climate upon North Atlantic Deep Water Formation in a Simple Ocean–Atmosphere Model 

    Source: Journal of Climate:;1997:;volume( 010 ):;issue: 001:;page 37
    Author(s): Winton, Michael
    Publisher: American Meteorological Society
    Abstract: The sensitivity of North Atlantic Deep Water formation to variations in mean surface temperature is explored with a meridional-vertical plane ocean model coupled to an energy balance atmosphere. It is found that North ...
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    The Damping Effect of Bottom Topography on Internal Decadal-Scale Oscillations of the Thermohaline Circulation 

    Source: Journal of Physical Oceanography:;1997:;Volume( 027 ):;issue: 001:;page 203
    Author(s): Winton, Michael
    Publisher: American Meteorological Society
    Abstract: By comparing the response of flat and bowl-shaped basins to fixed heat fluxes of various magnitudes, it is determined that coastal topography has a considerable damping influence upon internal decadal oscillations of the ...
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    Why Is the Deep Sinking Narrow? 

    Source: Journal of Physical Oceanography:;1995:;Volume( 025 ):;issue: 005:;page 997
    Author(s): Winton, Michael
    Publisher: American Meteorological Society
    Abstract: Narrowness of downwelling and broadness of upwelling are ubiquitous features of numerical and laboratory simulations of oceanic thermal overturning and are evidenced by the global ocean distributions of tracers, heat, and ...
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    Energetics of Deep-Decoupling Oscillations 

    Source: Journal of Physical Oceanography:;1995:;Volume( 025 ):;issue: 003:;page 420
    Author(s): Winton, Michael
    Publisher: American Meteorological Society
    Abstract: A number of single-hemisphere ocean models, when forced with steady mixed boundary conditions, have produced self-sustaining oscillations with century to millennial scale periods. Here the energetics of these deep-decoupling ...
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    On the Climatic Impact of Ocean Circulation 

    Source: Journal of Climate:;2003:;volume( 016 ):;issue: 017:;page 2875
    Author(s): Winton, Michael
    Publisher: American Meteorological Society
    Abstract: Integrations of coupled climate models with mixed-layer and fixed-current ocean components are used to explore the climatic response to varying magnitudes of ocean circulation. Four mixed-layer ocean experiments without ...
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    A Reformulated Three-Layer Sea Ice Model 

    Source: Journal of Atmospheric and Oceanic Technology:;2000:;volume( 017 ):;issue: 004:;page 525
    Author(s): Winton, Michael
    Publisher: American Meteorological Society
    Abstract: A model is presented that provides an efficient approximation to sea ice thermodynamics for climate studies. Semtner?s three-layer framework is used, but the brine content of the upper ice is represented with a variable ...
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    Simple Optical Models for Diagnosing Surface–Atmosphere Shortwave Interactions 

    Source: Journal of Climate:;2005:;volume( 018 ):;issue: 018:;page 3796
    Author(s): Winton, Michael
    Publisher: American Meteorological Society
    Abstract: A technique is developed for diagnosing effective surface and atmospheric optical properties from climate model shortwave flux diagnostics. These properties can be used to distinguish the contributions of surface and ...
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    Surface Albedo Feedback Estimates for the AR4 Climate Models 

    Source: Journal of Climate:;2006:;volume( 019 ):;issue: 003:;page 359
    Author(s): Winton, Michael
    Publisher: American Meteorological Society
    Abstract: A technique for estimating surface albedo feedback (SAF) from standard monthly mean climate model diagnostics is applied to the 1% yr?1 carbon dioxide (CO2)-increase transient climate change integrations of 12 Intergovernmental ...
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    Do Climate Models Underestimate the Sensitivity of Northern Hemisphere Sea Ice Cover? 

    Source: Journal of Climate:;2011:;volume( 024 ):;issue: 015:;page 3924
    Author(s): Winton, Michael
    Publisher: American Meteorological Society
    Abstract: he sensitivity of Northern Hemisphere sea ice cover to global temperature change is examined in a group of climate models and in the satellite-era observations. The models are found to have well-defined, distinguishable ...
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