Evaluation of Sea Ice Radiative Forcing according to Surface Albedo and Skin Temperature over the Ar...
Evaluation of Sea Ice Radiative Forcing according to Surface Albedo and Skin Temperature over the Arctic from 1982–2015
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Basel: MDPI AG
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Language
English
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Basel: MDPI AG
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Rapid warming of the Arctic has resulted in widespread sea ice loss. Sea ice radiative forcing (SIRF) is the instantaneous perturbation of Earth’s radiation at the top of the atmosphere (TOA) caused by sea ice. Previous studies focused only on the role of albedo on SIRF. Skin temperature is also closely related to sea ice changes and is one of the...
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Full title
Evaluation of Sea Ice Radiative Forcing according to Surface Albedo and Skin Temperature over the Arctic from 1982–2015
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TN_cdi_doaj_primary_oai_doaj_org_article_4199ce6a09274ed78b457e7da12cbed6
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https://devfeature-collection.sl.nsw.gov.au/record/TN_cdi_doaj_primary_oai_doaj_org_article_4199ce6a09274ed78b457e7da12cbed6
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ISSN
2072-4292
E-ISSN
2072-4292
DOI
10.3390/rs14112512
