Validity of the Ice Shelf Water plume concept under Filchner-Ronne Ice Shelf

In winter, brine rejection from sea ice formation and export in the Weddell Sea, offshore of Filchner-Ronne Ice Shelf (FRIS), leads to the formation of High Salinity Shelf Water (HSSW). This dense water mass enters the cavity beneath FRIS by sinking southward down the sloping continental shelf towar...

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Main Authors: Paul R. Holl, Daniel L. Feltham, Adrian Jenkins
Other Authors: The Pennsylvania State University CiteSeerX Archives
Format: Text
Language:English
Subjects:
Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.574.1557
http://www.cpom.org/people/dlf/holland_etal06.pdf
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spelling ftciteseerx:oai:CiteSeerX.psu:10.1.1.574.1557 2023-05-15T16:13:14+02:00 Validity of the Ice Shelf Water plume concept under Filchner-Ronne Ice Shelf Paul R. Holl Daniel L. Feltham Adrian Jenkins The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.574.1557 http://www.cpom.org/people/dlf/holland_etal06.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.574.1557 http://www.cpom.org/people/dlf/holland_etal06.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://www.cpom.org/people/dlf/holland_etal06.pdf text ftciteseerx 2016-01-08T12:40:14Z In winter, brine rejection from sea ice formation and export in the Weddell Sea, offshore of Filchner-Ronne Ice Shelf (FRIS), leads to the formation of High Salinity Shelf Water (HSSW). This dense water mass enters the cavity beneath FRIS by sinking southward down the sloping continental shelf towards the grounding line. Melting occurs when the Text Filchner Ronne Ice Shelf Filchner-Ronne Ice Shelf Ice Shelf Ronne Ice Shelf Sea ice Weddell Sea Unknown Ronne Ice Shelf ENVELOPE(-61.000,-61.000,-78.500,-78.500) Weddell Weddell Sea
institution Open Polar
collection Unknown
op_collection_id ftciteseerx
language English
description In winter, brine rejection from sea ice formation and export in the Weddell Sea, offshore of Filchner-Ronne Ice Shelf (FRIS), leads to the formation of High Salinity Shelf Water (HSSW). This dense water mass enters the cavity beneath FRIS by sinking southward down the sloping continental shelf towards the grounding line. Melting occurs when the
author2 The Pennsylvania State University CiteSeerX Archives
format Text
author Paul R. Holl
Daniel L. Feltham
Adrian Jenkins
spellingShingle Paul R. Holl
Daniel L. Feltham
Adrian Jenkins
Validity of the Ice Shelf Water plume concept under Filchner-Ronne Ice Shelf
author_facet Paul R. Holl
Daniel L. Feltham
Adrian Jenkins
author_sort Paul R. Holl
title Validity of the Ice Shelf Water plume concept under Filchner-Ronne Ice Shelf
title_short Validity of the Ice Shelf Water plume concept under Filchner-Ronne Ice Shelf
title_full Validity of the Ice Shelf Water plume concept under Filchner-Ronne Ice Shelf
title_fullStr Validity of the Ice Shelf Water plume concept under Filchner-Ronne Ice Shelf
title_full_unstemmed Validity of the Ice Shelf Water plume concept under Filchner-Ronne Ice Shelf
title_sort validity of the ice shelf water plume concept under filchner-ronne ice shelf
url http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.574.1557
http://www.cpom.org/people/dlf/holland_etal06.pdf
long_lat ENVELOPE(-61.000,-61.000,-78.500,-78.500)
geographic Ronne Ice Shelf
Weddell
Weddell Sea
geographic_facet Ronne Ice Shelf
Weddell
Weddell Sea
genre Filchner Ronne Ice Shelf
Filchner-Ronne Ice Shelf
Ice Shelf
Ronne Ice Shelf
Sea ice
Weddell Sea
genre_facet Filchner Ronne Ice Shelf
Filchner-Ronne Ice Shelf
Ice Shelf
Ronne Ice Shelf
Sea ice
Weddell Sea
op_source http://www.cpom.org/people/dlf/holland_etal06.pdf
op_relation http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.574.1557
http://www.cpom.org/people/dlf/holland_etal06.pdf
op_rights Metadata may be used without restrictions as long as the oai identifier remains attached to it.
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