Mechanisms delaying glacier retreat in the presence of ocean temperature variability at Thwaites Glacier, Antarctica [Slides]

In this work, we conclude ocean temperature variability affects grounding line evolution and glacier mass loss. As a consequence of local ocean density structure and bathymetry, variable runs always retreat less than steady runs.

Bibliographic Details
Main Author: Hoffman, Matthew James
Language:unknown
Published: 2023
Subjects:
58 GEOSCIENCES
54 ENVIRONMENTAL SCIENCES
97 MATHEMATICS AND COMPUTING
Thwaites Glacier
Antarc*
Antarctica
Online Access:http://www.osti.gov/servlets/purl/1814744
https://www.osti.gov/biblio/1814744
https://doi.org/10.2172/1814744
id ftosti:oai:osti.gov:1814744
record_format openpolar
spelling ftosti:oai:osti.gov:1814744 2023-07-30T03:57:39+02:00 Mechanisms delaying glacier retreat in the presence of ocean temperature variability at Thwaites Glacier, Antarctica [Slides] Hoffman, Matthew James 2023-01-24 application/pdf http://www.osti.gov/servlets/purl/1814744 https://www.osti.gov/biblio/1814744 https://doi.org/10.2172/1814744 unknown http://www.osti.gov/servlets/purl/1814744 https://www.osti.gov/biblio/1814744 https://doi.org/10.2172/1814744 doi:10.2172/1814744 58 GEOSCIENCES 54 ENVIRONMENTAL SCIENCES 97 MATHEMATICS AND COMPUTING 2023 ftosti https://doi.org/10.2172/1814744 2023-07-11T10:06:20Z In this work, we conclude ocean temperature variability affects grounding line evolution and glacier mass loss. As a consequence of local ocean density structure and bathymetry, variable runs always retreat less than steady runs. Other/Unknown Material Antarc* Antarctica Thwaites Glacier SciTec Connect (Office of Scientific and Technical Information - OSTI, U.S. Department of Energy) Thwaites Glacier ENVELOPE(-106.750,-106.750,-75.500,-75.500)
institution Open Polar
collection SciTec Connect (Office of Scientific and Technical Information - OSTI, U.S. Department of Energy)
op_collection_id ftosti
language unknown
topic 58 GEOSCIENCES
54 ENVIRONMENTAL SCIENCES
97 MATHEMATICS AND COMPUTING
spellingShingle 58 GEOSCIENCES
54 ENVIRONMENTAL SCIENCES
97 MATHEMATICS AND COMPUTING
Hoffman, Matthew James
Mechanisms delaying glacier retreat in the presence of ocean temperature variability at Thwaites Glacier, Antarctica [Slides]
topic_facet 58 GEOSCIENCES
54 ENVIRONMENTAL SCIENCES
97 MATHEMATICS AND COMPUTING
description In this work, we conclude ocean temperature variability affects grounding line evolution and glacier mass loss. As a consequence of local ocean density structure and bathymetry, variable runs always retreat less than steady runs.
author Hoffman, Matthew James
author_facet Hoffman, Matthew James
author_sort Hoffman, Matthew James
title Mechanisms delaying glacier retreat in the presence of ocean temperature variability at Thwaites Glacier, Antarctica [Slides]
title_short Mechanisms delaying glacier retreat in the presence of ocean temperature variability at Thwaites Glacier, Antarctica [Slides]
title_full Mechanisms delaying glacier retreat in the presence of ocean temperature variability at Thwaites Glacier, Antarctica [Slides]
title_fullStr Mechanisms delaying glacier retreat in the presence of ocean temperature variability at Thwaites Glacier, Antarctica [Slides]
title_full_unstemmed Mechanisms delaying glacier retreat in the presence of ocean temperature variability at Thwaites Glacier, Antarctica [Slides]
title_sort mechanisms delaying glacier retreat in the presence of ocean temperature variability at thwaites glacier, antarctica [slides]
publishDate 2023
url http://www.osti.gov/servlets/purl/1814744
https://www.osti.gov/biblio/1814744
https://doi.org/10.2172/1814744
long_lat ENVELOPE(-106.750,-106.750,-75.500,-75.500)
geographic Thwaites Glacier
geographic_facet Thwaites Glacier
genre Antarc*
Antarctica
Thwaites Glacier
genre_facet Antarc*
Antarctica
Thwaites Glacier
op_relation http://www.osti.gov/servlets/purl/1814744
https://www.osti.gov/biblio/1814744
https://doi.org/10.2172/1814744
doi:10.2172/1814744
op_doi https://doi.org/10.2172/1814744
_version_ 1772818642468077568

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