Abstract-The formation of fast ice in the costal zone of freezing seas (immobile ice) is considered on the basis of a specially developed thermodynamic model that takes into account the energy exchange in the atmo spheric boundary layer and the salinification of the water layer under the ice. The co...

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Main Authors: P V Bogorodskii, A V Marchenko, A V Pnyushkov, S A Ogorodov
Other Authors: The Pennsylvania State University CiteSeerX Archives
Format: Text
Language:English
Subjects:
Kara Sea
Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.1068.2404
http://www.geogr.msu.ru/structure/labs/geos/personal/Bogorodskii2010.pdf
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spelling ftciteseerx:oai:CiteSeerX.psu:10.1.1.1068.2404 2023-05-15T16:59:52+02:00 P V Bogorodskii A V Marchenko A V Pnyushkov S A Ogorodov The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.1068.2404 http://www.geogr.msu.ru/structure/labs/geos/personal/Bogorodskii2010.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.1068.2404 http://www.geogr.msu.ru/structure/labs/geos/personal/Bogorodskii2010.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://www.geogr.msu.ru/structure/labs/geos/personal/Bogorodskii2010.pdf text ftciteseerx 2020-04-26T00:15:25Z Abstract-The formation of fast ice in the costal zone of freezing seas (immobile ice) is considered on the basis of a specially developed thermodynamic model that takes into account the energy exchange in the atmo spheric boundary layer and the salinification of the water layer under the ice. The conditions at which the wind forced onshore motion of the ice under the influence of the wind stress at the ice's surface is possible are studied using the example of the Baidaratskaya Guba in the Kara Sea. Text Kara Sea Unknown Kara Sea
institution Open Polar
collection Unknown
op_collection_id ftciteseerx
language English
description Abstract-The formation of fast ice in the costal zone of freezing seas (immobile ice) is considered on the basis of a specially developed thermodynamic model that takes into account the energy exchange in the atmo spheric boundary layer and the salinification of the water layer under the ice. The conditions at which the wind forced onshore motion of the ice under the influence of the wind stress at the ice's surface is possible are studied using the example of the Baidaratskaya Guba in the Kara Sea.
author2 The Pennsylvania State University CiteSeerX Archives
format Text
author P V Bogorodskii
A V Marchenko
A V Pnyushkov
S A Ogorodov
spellingShingle P V Bogorodskii
A V Marchenko
A V Pnyushkov
S A Ogorodov
author_facet P V Bogorodskii
A V Marchenko
A V Pnyushkov
S A Ogorodov
author_sort P V Bogorodskii
url http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.1068.2404
http://www.geogr.msu.ru/structure/labs/geos/personal/Bogorodskii2010.pdf
geographic Kara Sea
geographic_facet Kara Sea
genre Kara Sea
genre_facet Kara Sea
op_source http://www.geogr.msu.ru/structure/labs/geos/personal/Bogorodskii2010.pdf
op_relation http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.1068.2404
http://www.geogr.msu.ru/structure/labs/geos/personal/Bogorodskii2010.pdf
op_rights Metadata may be used without restrictions as long as the oai identifier remains attached to it.
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