On the surface circulation in some channels of the Canadian Arctic Archipelago. Arctic

ABSTRACT. This paper advances an explanation for the presence of surface currents in opposite directions on facing sides of some of the main channels of the Canadian Arctic Archipelago. It is found that geostrophic dynamics coupled with geometrical constraints and the general direction of surface dr...

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Main Author: Paul H. Leblond
Other Authors: The Pennsylvania State University CiteSeerX Archives
Format: Text
Language:English
Published: 1980
Subjects:
Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.497.4132
http://pubs.aina.ucalgary.ca/arctic/Arctic33-1-189.pdf
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spelling ftciteseerx:oai:CiteSeerX.psu:10.1.1.497.4132 2023-05-15T14:19:51+02:00 On the surface circulation in some channels of the Canadian Arctic Archipelago. Arctic Paul H. Leblond The Pennsylvania State University CiteSeerX Archives 1980 application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.497.4132 http://pubs.aina.ucalgary.ca/arctic/Arctic33-1-189.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.497.4132 http://pubs.aina.ucalgary.ca/arctic/Arctic33-1-189.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://pubs.aina.ucalgary.ca/arctic/Arctic33-1-189.pdf text 1980 ftciteseerx 2016-01-08T08:51:07Z ABSTRACT. This paper advances an explanation for the presence of surface currents in opposite directions on facing sides of some of the main channels of the Canadian Arctic Archipelago. It is found that geostrophic dynamics coupled with geometrical constraints and the general direction of surface drift through the archipelago can readily account for the existence, if not all the properties, of the observed flow patterns. Text Arctic Arctic Archipelago Arctic Canadian Arctic Archipelago Unknown Arctic Canadian Arctic Archipelago
institution Open Polar
collection Unknown
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language English
description ABSTRACT. This paper advances an explanation for the presence of surface currents in opposite directions on facing sides of some of the main channels of the Canadian Arctic Archipelago. It is found that geostrophic dynamics coupled with geometrical constraints and the general direction of surface drift through the archipelago can readily account for the existence, if not all the properties, of the observed flow patterns.
author2 The Pennsylvania State University CiteSeerX Archives
format Text
author Paul H. Leblond
spellingShingle Paul H. Leblond
On the surface circulation in some channels of the Canadian Arctic Archipelago. Arctic
author_facet Paul H. Leblond
author_sort Paul H. Leblond
title On the surface circulation in some channels of the Canadian Arctic Archipelago. Arctic
title_short On the surface circulation in some channels of the Canadian Arctic Archipelago. Arctic
title_full On the surface circulation in some channels of the Canadian Arctic Archipelago. Arctic
title_fullStr On the surface circulation in some channels of the Canadian Arctic Archipelago. Arctic
title_full_unstemmed On the surface circulation in some channels of the Canadian Arctic Archipelago. Arctic
title_sort on the surface circulation in some channels of the canadian arctic archipelago. arctic
publishDate 1980
url http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.497.4132
http://pubs.aina.ucalgary.ca/arctic/Arctic33-1-189.pdf
geographic Arctic
Canadian Arctic Archipelago
geographic_facet Arctic
Canadian Arctic Archipelago
genre Arctic
Arctic Archipelago
Arctic
Canadian Arctic Archipelago
genre_facet Arctic
Arctic Archipelago
Arctic
Canadian Arctic Archipelago
op_source http://pubs.aina.ucalgary.ca/arctic/Arctic33-1-189.pdf
op_relation http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.497.4132
http://pubs.aina.ucalgary.ca/arctic/Arctic33-1-189.pdf
op_rights Metadata may be used without restrictions as long as the oai identifier remains attached to it.
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