Examining micropaleontology to gain insights into long-term processes in the Western Amundsen Sea, Antarctica
MS student, Coastal & Marine Science Systems, Department of Physical and Environmental Sciences AIS is divided into two ice sheets, the . (WAIS) and the east. AIS has exhibited rapid mass loss over the past two decades, with the most pronounced changes observed in the West Antarctic Ice Sheet (S...
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fttexasamucorpus:oai:tamucc-ir.tdl.org:1969.6/97544 2023-11-12T04:00:51+01:00 Examining micropaleontology to gain insights into long-term processes in the Western Amundsen Sea, Antarctica Szemak, Magkena 2023-08-30 application/vnd.openxmlformats-officedocument.presentationml.presentation https://hdl.handle.net/1969.6/97544 en_US eng https://hdl.handle.net/1969.6/97544 Presentation 2023 fttexasamucorpus 2023-10-14T22:07:09Z MS student, Coastal & Marine Science Systems, Department of Physical and Environmental Sciences AIS is divided into two ice sheets, the . (WAIS) and the east. AIS has exhibited rapid mass loss over the past two decades, with the most pronounced changes observed in the West Antarctic Ice Sheet (Shepherd et al., 2018). And because this is where my study site is located I’m going to focus there. WiAIS has a few unique physical characteristics, its much …Which make it highly vulnerable to changes in ocean currents or water temperature. The largest threat facing this region is Circumpolar Deep Water. As CDW is the greatest contributor of ice loss in this region, understanding the history of CDW movement and past deglaciation is critical to understanding the future! Conference Object Amundsen Sea Antarc* Antarctic Antarctica Ice Sheet Texas A&M University - Corpus Christi: DSpace Repository Amundsen Sea Antarctic West Antarctic Ice Sheet |
institution |
Open Polar |
collection |
Texas A&M University - Corpus Christi: DSpace Repository |
op_collection_id |
fttexasamucorpus |
language |
English |
description |
MS student, Coastal & Marine Science Systems, Department of Physical and Environmental Sciences AIS is divided into two ice sheets, the . (WAIS) and the east. AIS has exhibited rapid mass loss over the past two decades, with the most pronounced changes observed in the West Antarctic Ice Sheet (Shepherd et al., 2018). And because this is where my study site is located I’m going to focus there. WiAIS has a few unique physical characteristics, its much …Which make it highly vulnerable to changes in ocean currents or water temperature. The largest threat facing this region is Circumpolar Deep Water. As CDW is the greatest contributor of ice loss in this region, understanding the history of CDW movement and past deglaciation is critical to understanding the future! |
format |
Conference Object |
author |
Szemak, Magkena |
spellingShingle |
Szemak, Magkena Examining micropaleontology to gain insights into long-term processes in the Western Amundsen Sea, Antarctica |
author_facet |
Szemak, Magkena |
author_sort |
Szemak, Magkena |
title |
Examining micropaleontology to gain insights into long-term processes in the Western Amundsen Sea, Antarctica |
title_short |
Examining micropaleontology to gain insights into long-term processes in the Western Amundsen Sea, Antarctica |
title_full |
Examining micropaleontology to gain insights into long-term processes in the Western Amundsen Sea, Antarctica |
title_fullStr |
Examining micropaleontology to gain insights into long-term processes in the Western Amundsen Sea, Antarctica |
title_full_unstemmed |
Examining micropaleontology to gain insights into long-term processes in the Western Amundsen Sea, Antarctica |
title_sort |
examining micropaleontology to gain insights into long-term processes in the western amundsen sea, antarctica |
publishDate |
2023 |
url |
https://hdl.handle.net/1969.6/97544 |
geographic |
Amundsen Sea Antarctic West Antarctic Ice Sheet |
geographic_facet |
Amundsen Sea Antarctic West Antarctic Ice Sheet |
genre |
Amundsen Sea Antarc* Antarctic Antarctica Ice Sheet |
genre_facet |
Amundsen Sea Antarc* Antarctic Antarctica Ice Sheet |
op_relation |
https://hdl.handle.net/1969.6/97544 |
_version_ |
1782328891296186368 |