The Albedo of Sea-Ice and Ice Islands in the Arctic Ocean Basin

T HE surface albedo * and its change during the spring, summer and autumn seasons is probably the most significant regional factor affect-ing the heat budget of the Arctic Ocean basin. In the spring, when most of the sea-ice is covered with snow, the albedo of the surface is between 80 and 90 per ce...

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Main Author: Kirby J. Hanson
Other Authors: The Pennsylvania State University CiteSeerX Archives
Format: Text
Language:English
Published: 1961
Subjects:
Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.483.3422
http://pubs.aina.ucalgary.ca/arctic/Arctic14-3-188.pdf
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spelling ftciteseerx:oai:CiteSeerX.psu:10.1.1.483.3422 2023-05-15T13:10:23+02:00 The Albedo of Sea-Ice and Ice Islands in the Arctic Ocean Basin Kirby J. Hanson The Pennsylvania State University CiteSeerX Archives 1961 application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.483.3422 http://pubs.aina.ucalgary.ca/arctic/Arctic14-3-188.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.483.3422 http://pubs.aina.ucalgary.ca/arctic/Arctic14-3-188.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://pubs.aina.ucalgary.ca/arctic/Arctic14-3-188.pdf text 1961 ftciteseerx 2016-01-08T08:02:12Z T HE surface albedo * and its change during the spring, summer and autumn seasons is probably the most significant regional factor affect-ing the heat budget of the Arctic Ocean basin. In the spring, when most of the sea-ice is covered with snow, the albedo of the surface is between 80 and 90 per cent. In mid-summer, however, the snow cover melts, fairly Text albedo Arctic Arctic Arctic Ocean Sea ice Unknown Arctic Arctic Ocean
institution Open Polar
collection Unknown
op_collection_id ftciteseerx
language English
description T HE surface albedo * and its change during the spring, summer and autumn seasons is probably the most significant regional factor affect-ing the heat budget of the Arctic Ocean basin. In the spring, when most of the sea-ice is covered with snow, the albedo of the surface is between 80 and 90 per cent. In mid-summer, however, the snow cover melts, fairly
author2 The Pennsylvania State University CiteSeerX Archives
format Text
author Kirby J. Hanson
spellingShingle Kirby J. Hanson
The Albedo of Sea-Ice and Ice Islands in the Arctic Ocean Basin
author_facet Kirby J. Hanson
author_sort Kirby J. Hanson
title The Albedo of Sea-Ice and Ice Islands in the Arctic Ocean Basin
title_short The Albedo of Sea-Ice and Ice Islands in the Arctic Ocean Basin
title_full The Albedo of Sea-Ice and Ice Islands in the Arctic Ocean Basin
title_fullStr The Albedo of Sea-Ice and Ice Islands in the Arctic Ocean Basin
title_full_unstemmed The Albedo of Sea-Ice and Ice Islands in the Arctic Ocean Basin
title_sort albedo of sea-ice and ice islands in the arctic ocean basin
publishDate 1961
url http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.483.3422
http://pubs.aina.ucalgary.ca/arctic/Arctic14-3-188.pdf
geographic Arctic
Arctic Ocean
geographic_facet Arctic
Arctic Ocean
genre albedo
Arctic
Arctic
Arctic Ocean
Sea ice
genre_facet albedo
Arctic
Arctic
Arctic Ocean
Sea ice
op_source http://pubs.aina.ucalgary.ca/arctic/Arctic14-3-188.pdf
op_relation http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.483.3422
http://pubs.aina.ucalgary.ca/arctic/Arctic14-3-188.pdf
op_rights Metadata may be used without restrictions as long as the oai identifier remains attached to it.
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