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GEOPHYSICAL RESEARCH LETTERS,
VOL. 35,
L08503,
doi:10.1029/2008GL033451,
2008
The contribution of cloud and radiation anomalies to the 2007 Arctic sea ice extent minimum
Jennifer E. Kay
Climate and Global Dynamics Division, National Center for Atmospheric Research, Boulder, Colorado, USA Department of Atmospheric Sciences, Colorado State University, Fort Collins, Colorado, USA
Tristan L'Ecuyer
Department of Atmospheric Sciences, Colorado State University, Fort Collins, Colorado, USA
Andrew Gettelman
Climate and Global Dynamics Division, National Center for Atmospheric Research, Boulder, Colorado, USA
Graeme Stephens
Department of Atmospheric Sciences, Colorado State University, Fort Collins, Colorado, USA
Chris O'Dell
Department of Atmospheric Sciences, Colorado State University, Fort Collins, Colorado, USA
Abstract
Reduced cloudiness and enhanced downwelling radiation are associated with the unprecedented 2007 Arctic sea ice loss. Over
the Western Arctic Ocean, total summertime cloud cover estimated from spaceborne radar and lidar data decreased by 16% from
2006 to 2007. The clearer skies led to downwelling shortwave (longwave) radiative fluxes increases of +32 Wm−2 (−4 Wm−2) from 2006 to 2007. Over three months, simple calculations show that these radiation differences alone could enhance surface
ice melt by 0.3 m, or warm the surface ocean by 2.4 K, which enhances basal ice melt. Increased air temperatures and decreased
relative humidity associated with an anti-cyclonic atmospheric circulation pattern explain the reduced cloudiness. Longer-term
observations show that the 2007 cloudiness is anomalous in the recent past, but is not unprecedented. Thus, in a warmer world
with thinner ice, natural summertime circulation and cloud variability is an increasingly important control on sea ice extent
minima.
Received 29
January
2008;
accepted 13
March
2008;
published 22
April
2008.
Keywords: Arctic sea ice;
radiation;
clouds.
Index Terms: 1621 Global Change: Cryospheric change (0776); 1610 Global Change: Atmosphere (0315, 0325); 1640 Global Change: Remote sensing (1855); 3310 Atmospheric Processes: Clouds and cloud feedbacks; 3349 Atmospheric Processes: Polar meteorology.
Read Full Article (file size: 1580925 bytes) Cited by
Citation: Kay, J. E., T. L'Ecuyer, A. Gettelman, G. Stephens, and C. O'Dell
(2008),
The contribution of cloud and radiation anomalies to the 2007 Arctic sea ice extent minimum,
Geophys. Res. Lett.,
35,
L08503,
doi:10.1029/2008GL033451.
Copyright 2008 by the American Geophysical Union.
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