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    Impacts of Stratospheric Ozone Extremes on Arctic High Cloud 

    Source: Journal of Climate:;2020:;volume( 33 ):;issue: 020:;page 8869
    Author(s): Maleska, Sarah;Smith, Karen L.;Virgin, John
    Publisher: American Meteorological Society
    Abstract: Stratospheric ozone depletion in the Antarctic is well known to cause changes in Southern Hemisphere tropospheric climate; however, because of its smaller magnitude in the Arctic, the effects of stratospheric ozone depletion ...
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    No Surface Cooling over Antarctica from the Negative Greenhouse Effect Associated with Instantaneous Quadrupling of CO2 Concentrations 

    Source: Journal of Climate:;2017:;volume( 031 ):;issue: 001:;page 317
    Author(s): Smith, Karen L.;Chiodo, Gabriel;Previdi, Michael;Polvani, Lorenzo M.
    Publisher: American Meteorological Society
    Abstract: AbstractOver the highest elevations of Antarctica, during many months of the year, air near the surface is colder than in much of the overlying atmosphere. This unique feature of the Antarctic atmosphere has been shown to ...
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    The Role of Linear Interference in the Annular Mode Response to Extratropical Surface Forcing 

    Source: Journal of Climate:;2010:;volume( 023 ):;issue: 022:;page 6036
    Author(s): Smith, Karen L.; Fletcher, Christopher G.; Kushner, Paul J.
    Publisher: American Meteorological Society
    Abstract: The classical problem of predicting the atmospheric circulation response to extratropical surface forcing is revisited in the context of the observed connection between autumnal snow cover anomalies over Siberia and ...
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    The Antarctic Atmospheric Energy Budget. Part I: Climatology and Intraseasonal-to-Interannual Variability 

    Source: Journal of Climate:;2013:;volume( 026 ):;issue: 017:;page 6406
    Author(s): Previdi, Michael; Smith, Karen L.; Polvani, Lorenzo M.
    Publisher: American Meteorological Society
    Abstract: he authors present a new, observationally based estimate of the atmospheric energy budget for the Antarctic polar cap (the region poleward of 70°S). This energy budget is constructed using state-of-the-art reanalysis ...
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    The Antarctic Atmospheric Energy Budget. Part II: The Effect of Ozone Depletion and its Projected Recovery 

    Source: Journal of Climate:;2013:;volume( 026 ):;issue: 024:;page 9729
    Author(s): Smith, Karen L.; Previdi, Michael; Polvani, Lorenzo M.
    Publisher: American Meteorological Society
    Abstract: n this study the authors continue their investigation of the atmospheric energy budget of the Antarctic polar cap (the region poleward of 70°S) using integrations of the Whole Atmosphere Community Climate Model from the ...
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    The Role of Linear Interference in Northern Annular Mode Variability Associated with Eurasian Snow Cover Extent 

    Source: Journal of Climate:;2011:;volume( 024 ):;issue: 023:;page 6185
    Author(s): Smith, Karen L.; Kushner, Paul J.; Cohen, Judah
    Publisher: American Meteorological Society
    Abstract: ne of the outstanding questions regarding the observed relationship between October Eurasian snow cover anomalies and the boreal winter northern annular mode (NAM) is what causes the multiple-week lag between positive ...
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    How Well Do the CMIP5 Models Simulate the Antarctic Atmospheric Energy Budget? 

    Source: Journal of Climate:;2015:;volume( 028 ):;issue: 020:;page 7933
    Author(s): Previdi, Michael; Smith, Karen L.; Polvani, Lorenzo M.
    Publisher: American Meteorological Society
    Abstract: he authors evaluate 23 coupled atmosphere?ocean general circulation models from phase 5 of CMIP (CMIP5) in terms of their ability to simulate the observed climatological mean energy budget of the Antarctic atmosphere. While ...
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    The Impact of Stratospheric Circulation Extremes on Minimum Arctic Sea Ice Extent 

    Source: Journal of Climate:;2018:;volume 031:;issue 018:;page 7169
    Author(s): Smith, Karen L.; Polvani, Lorenzo M.; Tremblay, L. Bruno
    Publisher: American Meteorological Society
    Abstract: AbstractGiven the rapidly changing Arctic climate, there is an urgent need for improved seasonal predictions of Arctic sea ice. Yet, Arctic sea ice prediction is inherently complex. Among other factors, wintertime atmospheric ...
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    No Surface Cooling over Antarctica from the Negative Greenhouse Effect Associated with Instantaneous Quadrupling of CO2 Concentrations 

    Source: Journal of Climate:;2017:;volume 031:;issue 001:;page 317
    Author(s): Smith, Karen L.; Chiodo, Gabriel; Previdi, Michael; Polvani, Lorenzo M.
    Publisher: American Meteorological Society
    Abstract: AbstractOver the highest elevations of Antarctica, during many months of the year, air near the surface is colder than in much of the overlying atmosphere. This unique feature of the Antarctic atmosphere has been shown to ...
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    A Climatology of Tropospheric Zonal-Mean Water Vapor Fields and Fluxes in Isentropic Coordinates 

    Source: Journal of Climate:;2006:;volume( 019 ):;issue: 022:;page 5918
    Author(s): Schneider, Tapio; Smith, Karen L.; O’Gorman, Paul A.; Walker, Christopher C.
    Publisher: American Meteorological Society
    Abstract: Based on reanalysis data for the years 1980?2001 from the European Centre for Medium-Range Weather Forecasts (ERA-40 data), a climatology of tropospheric zonal-mean water vapor fields and fluxes in isentropic coordinates ...
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