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    A Mechanism for the High Rate of Sea Ice Thinning in the Arctic Ocean 

    Source: Journal of Climate:;2004:;volume( 017 ):;issue: 018:;page 3623
    Author(s): Bitz, C. M.; Roe, G. H.
    Publisher: American Meteorological Society
    Abstract: Submarine measurements of sea ice draft show that the ice has thinned in some parts of the Arctic Ocean at a remarkably high rate over the past few decades. The spatial pattern indicates that the thinning was a strong ...
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    Interannual to Decadal Variability in Climate and the Glacier Mass Balance in Washington, Western Canada, and Alaska 

    Source: Journal of Climate:;1999:;volume( 012 ):;issue: 011:;page 3181
    Author(s): Bitz, C. M.; Battisti, D. S.
    Publisher: American Meteorological Society
    Abstract: The authors examine the net winter, summer, and annual mass balance of six glaciers along the northwest coast of North America, extending from Washington State to Alaska. The net winter (NWB) and net annual (NAB) mass ...
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    Do General Circulation Models Underestimate the Natural Variability in the Arctic Climate? 

    Source: Journal of Climate:;1997:;volume( 010 ):;issue: 008:;page 1909
    Author(s): Battisti, D. S.; Bitz, C. M.; Moritz, R. E.
    Publisher: American Meteorological Society
    Abstract: The authors examine the natural variability of the arctic climate system simulated by two very different models: the Geophysical Fluid Dynamics Laboratory (GFDL) global climate model, and an area-averaged model of the ...
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    Sea Ice Response to Wind Forcing from AMIP Models 

    Source: Journal of Climate:;2002:;volume( 015 ):;issue: 005:;page 522
    Author(s): Bitz, C. M.; Fyfe, John C.; Flato, Gregory M.
    Publisher: American Meteorological Society
    Abstract: The Arctic surface circulation simulated by atmospheric general circulation models is assessed in the context of driving sea ice motion. A sea ice model is forced by geostrophic winds from eight models participating in the ...
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    Low-Frequency Variability in the Arctic Atmosphere, Sea Ice, and Upper-Ocean Climate System 

    Source: Journal of Climate:;1996:;volume( 009 ):;issue: 002:;page 394
    Author(s): Bitz, C. M.; Battisti, D. S.; Moritz, R. E.; Beesley, J. A.
    Publisher: American Meteorological Society
    Abstract: The low-frequency natural variability of the arctic climate system is modeled using a single-column, energy balance model of the atmosphere. sea ice, and upper-ocean system. Variability in the system is induced by forcing ...
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    Maintenance of the Sea-Ice Edge 

    Source: Journal of Climate:;2005:;volume( 018 ):;issue: 015:;page 2903
    Author(s): Bitz, C. M.; Holland, M. M.; Hunke, E. C.; Moritz, R. E.
    Publisher: American Meteorological Society
    Abstract: A coupled global climate model is used to evaluate processes that determine the equilibrium location of the sea-ice edge and its climatological annual cycle. The extent to which the wintertime ice edge departs from a ...
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    The Influence of Sea Ice on Ocean Heat Uptake in Response to Increasing CO2 

    Source: Journal of Climate:;2006:;volume( 019 ):;issue: 011:;page 2437
    Author(s): Bitz, C. M.; Gent, P. R.; Woodgate, R. A.; Holland, M. M.; Lindsay, R.
    Publisher: American Meteorological Society
    Abstract: Two significant changes in ocean heat uptake that occur in the vicinity of sea ice cover in response to increasing CO2 are investigated with Community Climate System Model version 3 (CCSM3): a deep warming below ?500 m and ...
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    CORRIGENDUM 

    Source: Journal of Climate:;2007:;volume( 020 ):;issue: 012:;page 2864
    Author(s): Bitz, C. M.; Gent, P. R.; Woodgate, R. A.; Holland, M. M.; Lindsay, R.
    Publisher: American Meteorological Society
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    Climate Sensitivity of the Community Climate System Model, Version 4 

    Source: Journal of Climate:;2011:;volume( 025 ):;issue: 009:;page 3053
    Author(s): Bitz, C. M.; Shell, K. M.; Gent, P. R.; Bailey, D. A.; Danabasoglu, G.; Armour, K. C.; Holland, M. M.; Kiehl, J. T.
    Publisher: American Meteorological Society
    Abstract: quilibrium climate sensitivity of the Community Climate System Model, version 4 (CCSM4) is 3.20°C for 1° horizontal resolution in each component. This is about a half degree Celsius higher than in the previous version ...
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