RADIATIVE FLUXES AND ALBEDO FEEDBACK IN POLAR REGIONS

dc.contributor.advisorPinker, Rachel T.en_US
dc.contributor.authorNiu, Xiaoleien_US
dc.contributor.departmentAtmospheric and Oceanic Sciencesen_US
dc.contributor.publisherDigital Repository at the University of Marylanden_US
dc.contributor.publisherUniversity of Maryland (College Park, Md.)en_US
dc.date.accessioned2012-02-17T07:11:34Z
dc.date.available2012-02-17T07:11:34Z
dc.date.issued2011en_US
dc.description.abstractThe Arctic is experiencing an unprecedented increase in surface temperature and decrease in sea ice extent. Discussion as to the causes that contribute to the Arctic warming is still ongoing. The ice-albedo feedback has been proposed as a possible mechanism for polar amplification of such warming. It states that more open water leads to more solar heat absorption, which results in more ice melting and more open water. In order to study this relationship there is a need for accurate information on the solar heat input into the Arctic Oceans. I have developed and improved inference schemes for shortwave radiative fluxes that respond to the needs of Polar Regions utilizing most recent information on atmospheric and surface states. A Moderate Resolution Imaging Spectroradiometer (MODIS) approach has been optimized for Polar Regions and implemented at 1&deg; for 2002-2010 and at 5-km for 2007. A methodology was developed to derive solar fluxes from the Advanced Very High Resolution Radiometer (AVHRR) and implemented at 0.5&deg; for 1983-2006. Evaluation against ground measurements over land and ocean at high latitudes shows that the MODIS shortwave flux estimates are in best agreement with ground observations as compared to other available satellite and model products, with a bias of -3.6 Wm<super>-2</super> and standard deviation of 23 Wm<super>-2</super> at a daily time scale. The AVHRR estimates agree with ground observations with a bias of -4.7 Wm<super>-2</super> and a standard deviation of 41 Wm<super>-2</super> at a daily time scale. The ice-albedo feedback was evaluated by computing the solar heating into the Arctic Ocean using the improved satellite flux estimates. A growth at a rate of 2 %/year in the trend of solar heating for 2003-09 was found at a 75 % confidence level; the trend for 1984-2002 was only 0.2 %/year at a 99 % confidence level. The ice retreat is correlated to the solar energy into the ocean at 0.7 at a 75 % confidence level. An increase in the open water fraction resulted in a maximum 300 % positive anomaly in solar heating in 2007 located where the maximum sea ice retreat is.en_US
dc.identifier.urihttp://hdl.handle.net/1903/12386
dc.subject.pqcontrolledAtmospheric sciencesen_US
dc.subject.pqcontrolledClimate changeen_US
dc.subject.pquncontrolledArctic sea ice lossen_US
dc.subject.pquncontrolledIce-albedo feedbacken_US
dc.subject.pquncontrolledPolar Regionen_US
dc.subject.pquncontrolledRadiationen_US
dc.subject.pquncontrolledRemote Sensingen_US
dc.titleRADIATIVE FLUXES AND ALBEDO FEEDBACK IN POLAR REGIONSen_US
dc.typeDissertationen_US

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