The Antarctic Coastal Current in the Bellingshausen Sea

The ice shelves in the Western Antarctic have seen an increase in melt over the past decade, mainly due to basal melting induced by underlying warm, salty Circumpolar Deep Water. Seal data in the Bellingshausen Sea provides extensive hydrographic coverage, allowing insight into a westward flowing co...

Full description

Bibliographic Details
Other Authors: Schubert, Ryan A. (author), Speer, Kevin G. (Kevin George) (professor directing thesis), Clarke, Allan J. (committee member), Bourassa, Mark Allan (committee member), Florida State University (degree granting institution), College of Arts and Sciences (degree granting college), Department of Earth, Ocean and Atmospheric Science (degree granting department)
Format: Master Thesis
Language:English
Published: Florida State University 2020
Subjects:
Online Access:https://diginole.lib.fsu.edu/islandora/object/fsu%3A777114/datastream/TN/view/Antarctic%20Coastal%20Current%20in%20the%20Bellingshausen%20Sea.jpg
id ftfloridasu:oai:diginole.lib.fsu.edu:fsu_777114
record_format openpolar
spelling ftfloridasu:oai:diginole.lib.fsu.edu:fsu_777114 2024-06-09T07:37:46+00:00 The Antarctic Coastal Current in the Bellingshausen Sea Schubert, Ryan A. (author) Speer, Kevin G. (Kevin George) (professor directing thesis) Clarke, Allan J. (committee member) Bourassa, Mark Allan (committee member) Florida State University (degree granting institution) College of Arts and Sciences (degree granting college) Department of Earth, Ocean and Atmospheric Science (degree granting department) 2020 computer online resource 1 online resource (63 pages) application/pdf https://diginole.lib.fsu.edu/islandora/object/fsu%3A777114/datastream/TN/view/Antarctic%20Coastal%20Current%20in%20the%20Bellingshausen%20Sea.jpg English eng Florida State University fsu:777114 iid: 2020_Summer_Fall_Schubert_fsu_0071N_16130 https://diginole.lib.fsu.edu/islandora/object/fsu%3A777114/datastream/TN/view/Antarctic%20Coastal%20Current%20in%20the%20Bellingshausen%20Sea.jpg Oceanography Text master thesis 2020 ftfloridasu 2024-05-10T08:08:10Z The ice shelves in the Western Antarctic have seen an increase in melt over the past decade, mainly due to basal melting induced by underlying warm, salty Circumpolar Deep Water. Seal data in the Bellingshausen Sea provides extensive hydrographic coverage, allowing insight into a westward flowing coastal current that acts to transport the meltwater. The observed coastal current enters the eastern Bellingshausen Sea from the Western Antarctic Peninsula, flowing westward along the coast to the Abbot Ice Shelf, where the fate of the current is unknown. The temperature and salinity profiles show that this coastal current has a baroclinic structure, that increases from east to west. While in the Bellingshausen Sea, the coastal current entrains meltwater from the ice shelves in the region, which increases the density grandient, increasing the westward transport of the current. The current acts as a mechanism to transport meltwater out of the Bellingshausen Sea and into the Amundsen Sea and Ross Sea, where it could impact the local melt rates and water mass formation. A Thesis submitted to the Department of Earth, Ocean, and Atmospheric Science in partial fulfillment of the requirements for the degree of Master of Science. July 13, 2020. Antarctic Coastal Current, Bellingshausen Sea, coastal current, Western Antarctic Includes bibliographical references. Kevin Speer, Professor Directing Thesis; Allan Clarke, Committee Member; Mark Bourassa, Committee Member. Master Thesis Abbot Ice Shelf Amundsen Sea Antarc* Antarctic Antarctic Peninsula Bellingshausen Sea Ice Shelf Ice Shelves Ross Sea Florida State University: DigiNole Commons Abbot Ice Shelf ENVELOPE(-96.000,-96.000,-72.750,-72.750) Amundsen Sea Antarctic Antarctic Peninsula Bellingshausen Sea Ross Sea The Antarctic
institution Open Polar
collection Florida State University: DigiNole Commons
op_collection_id ftfloridasu
language English
topic Oceanography
spellingShingle Oceanography
The Antarctic Coastal Current in the Bellingshausen Sea
topic_facet Oceanography
description The ice shelves in the Western Antarctic have seen an increase in melt over the past decade, mainly due to basal melting induced by underlying warm, salty Circumpolar Deep Water. Seal data in the Bellingshausen Sea provides extensive hydrographic coverage, allowing insight into a westward flowing coastal current that acts to transport the meltwater. The observed coastal current enters the eastern Bellingshausen Sea from the Western Antarctic Peninsula, flowing westward along the coast to the Abbot Ice Shelf, where the fate of the current is unknown. The temperature and salinity profiles show that this coastal current has a baroclinic structure, that increases from east to west. While in the Bellingshausen Sea, the coastal current entrains meltwater from the ice shelves in the region, which increases the density grandient, increasing the westward transport of the current. The current acts as a mechanism to transport meltwater out of the Bellingshausen Sea and into the Amundsen Sea and Ross Sea, where it could impact the local melt rates and water mass formation. A Thesis submitted to the Department of Earth, Ocean, and Atmospheric Science in partial fulfillment of the requirements for the degree of Master of Science. July 13, 2020. Antarctic Coastal Current, Bellingshausen Sea, coastal current, Western Antarctic Includes bibliographical references. Kevin Speer, Professor Directing Thesis; Allan Clarke, Committee Member; Mark Bourassa, Committee Member.
author2 Schubert, Ryan A. (author)
Speer, Kevin G. (Kevin George) (professor directing thesis)
Clarke, Allan J. (committee member)
Bourassa, Mark Allan (committee member)
Florida State University (degree granting institution)
College of Arts and Sciences (degree granting college)
Department of Earth, Ocean and Atmospheric Science (degree granting department)
format Master Thesis
title The Antarctic Coastal Current in the Bellingshausen Sea
title_short The Antarctic Coastal Current in the Bellingshausen Sea
title_full The Antarctic Coastal Current in the Bellingshausen Sea
title_fullStr The Antarctic Coastal Current in the Bellingshausen Sea
title_full_unstemmed The Antarctic Coastal Current in the Bellingshausen Sea
title_sort antarctic coastal current in the bellingshausen sea
publisher Florida State University
publishDate 2020
url https://diginole.lib.fsu.edu/islandora/object/fsu%3A777114/datastream/TN/view/Antarctic%20Coastal%20Current%20in%20the%20Bellingshausen%20Sea.jpg
long_lat ENVELOPE(-96.000,-96.000,-72.750,-72.750)
geographic Abbot Ice Shelf
Amundsen Sea
Antarctic
Antarctic Peninsula
Bellingshausen Sea
Ross Sea
The Antarctic
geographic_facet Abbot Ice Shelf
Amundsen Sea
Antarctic
Antarctic Peninsula
Bellingshausen Sea
Ross Sea
The Antarctic
genre Abbot Ice Shelf
Amundsen Sea
Antarc*
Antarctic
Antarctic Peninsula
Bellingshausen Sea
Ice Shelf
Ice Shelves
Ross Sea
genre_facet Abbot Ice Shelf
Amundsen Sea
Antarc*
Antarctic
Antarctic Peninsula
Bellingshausen Sea
Ice Shelf
Ice Shelves
Ross Sea
op_relation fsu:777114
iid: 2020_Summer_Fall_Schubert_fsu_0071N_16130
https://diginole.lib.fsu.edu/islandora/object/fsu%3A777114/datastream/TN/view/Antarctic%20Coastal%20Current%20in%20the%20Bellingshausen%20Sea.jpg
_version_ 1801371342945124352