The eect of McMurdo Sound topography on water mass exchange across the Ross Ice Shelf front

The southwestern Ross Sea continental shelf acts as formation site for highly dense shelf waters because of strong brine release due to vigorous sea ice production in the Ross Sea polynya (Jacobs & Guilivi 1998, Assmann et al. 2003). In this context it has been debated whether the topography of...

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Bibliographic Details
Main Author: Karen M. Assmann
Other Authors: The Pennsylvania State University CiteSeerX Archives
Format: Text
Language:English
Subjects:
McMurdo Sound
Ross Ice Shelf
Ross Sea
Ice Shelf
Sea ice
Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.508.1149
http://folk.uib.no/ngfls/frisp/Rep15/assmann.pdf
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spelling ftciteseerx:oai:CiteSeerX.psu:10.1.1.508.1149 2023-05-15T16:41:52+02:00 The eect of McMurdo Sound topography on water mass exchange across the Ross Ice Shelf front Karen M. Assmann The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.508.1149 http://folk.uib.no/ngfls/frisp/Rep15/assmann.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.508.1149 http://folk.uib.no/ngfls/frisp/Rep15/assmann.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://folk.uib.no/ngfls/frisp/Rep15/assmann.pdf text ftciteseerx 2016-01-08T09:28:21Z The southwestern Ross Sea continental shelf acts as formation site for highly dense shelf waters because of strong brine release due to vigorous sea ice production in the Ross Sea polynya (Jacobs & Guilivi 1998, Assmann et al. 2003). In this context it has been debated whether the topography of McMurdo Sound permits exchange with the Text Ice Shelf McMurdo Sound Ross Ice Shelf Ross Sea Sea ice Unknown McMurdo Sound Ross Ice Shelf Ross Sea
institution Open Polar
collection Unknown
op_collection_id ftciteseerx
language English
description The southwestern Ross Sea continental shelf acts as formation site for highly dense shelf waters because of strong brine release due to vigorous sea ice production in the Ross Sea polynya (Jacobs & Guilivi 1998, Assmann et al. 2003). In this context it has been debated whether the topography of McMurdo Sound permits exchange with the
author2 The Pennsylvania State University CiteSeerX Archives
format Text
author Karen M. Assmann
spellingShingle Karen M. Assmann
The eect of McMurdo Sound topography on water mass exchange across the Ross Ice Shelf front
author_facet Karen M. Assmann
author_sort Karen M. Assmann
title The eect of McMurdo Sound topography on water mass exchange across the Ross Ice Shelf front
title_short The eect of McMurdo Sound topography on water mass exchange across the Ross Ice Shelf front
title_full The eect of McMurdo Sound topography on water mass exchange across the Ross Ice Shelf front
title_fullStr The eect of McMurdo Sound topography on water mass exchange across the Ross Ice Shelf front
title_full_unstemmed The eect of McMurdo Sound topography on water mass exchange across the Ross Ice Shelf front
title_sort eect of mcmurdo sound topography on water mass exchange across the ross ice shelf front
url http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.508.1149
http://folk.uib.no/ngfls/frisp/Rep15/assmann.pdf
geographic McMurdo Sound
Ross Ice Shelf
Ross Sea
geographic_facet McMurdo Sound
Ross Ice Shelf
Ross Sea
genre Ice Shelf
McMurdo Sound
Ross Ice Shelf
Ross Sea
Sea ice
genre_facet Ice Shelf
McMurdo Sound
Ross Ice Shelf
Ross Sea
Sea ice
op_source http://folk.uib.no/ngfls/frisp/Rep15/assmann.pdf
op_relation http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.508.1149
http://folk.uib.no/ngfls/frisp/Rep15/assmann.pdf
op_rights Metadata may be used without restrictions as long as the oai identifier remains attached to it.
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