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Changes in summer sea ice, albedo, and portioning of surface solar radiation in the Pacific sector of Arctic Ocean during 1982-2009
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2016
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Source: Journal of Geophysical Research: Oceans, 121(8), 5470-5486
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Journal Title:Journal of Geophysical Research: Oceans
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Description:SSM/I sea ice concentration and CLARA black-sky composite albedo were used to estimate sea ice albedo in the region 70 8N–82 8N, 130 8W–180 8W. The long-term trends and seasonal evolutions of ice concentration, composite albedo, and ice albedo were then obtained. In July–August 1982–2009, the linear trend of the composite albedo and the ice albedo was 20.069 and 20.046 units per decade, respectively. During 1 June to 19 August, melting of sea ice resulted in an increase of solar heat input to the ice-oceansystem by 282 MJ /C1m 22from 1982 to 2009. However, because of the counter-balancing effects of the loss of sea ice area and the enhanced ice surface melting, the trend of solar heat input to the ice was insignificant.
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Source:Journal of Geophysical Research: Oceans, 121(8), 5470-5486
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ISSN:2169-9275
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Rights Information:Other
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Compliance:Library
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