Temporal Variations in Ice Thickness of the Shirase Glacier Derived from Cryosat-2/SIRAL Data

This study presents the feasibility of estimating the ice thickness of the Shirase Glacier using the synthetic aperture interferometric radar altimeter (SIRAL) on board the CryoSat-2 and the interannual variation of the ice thickness of the Shirase Glacier in 2011–2020. The SIRAL data were converted...

Full description

Bibliographic Details
Published in:Remote Sensing
Main Authors: Yurina Satake, Kazuki Nakamura
Format: Text
Language:English
Published: Multidisciplinary Digital Publishing Institute 2023
Subjects:
Online Access:https://doi.org/10.3390/rs15051205
id ftmdpi:oai:mdpi.com:/2072-4292/15/5/1205/
record_format openpolar
spelling ftmdpi:oai:mdpi.com:/2072-4292/15/5/1205/ 2023-08-20T04:09:47+02:00 Temporal Variations in Ice Thickness of the Shirase Glacier Derived from Cryosat-2/SIRAL Data Yurina Satake Kazuki Nakamura agris 2023-02-22 application/pdf https://doi.org/10.3390/rs15051205 EN eng Multidisciplinary Digital Publishing Institute Biogeosciences Remote Sensing https://dx.doi.org/10.3390/rs15051205 https://creativecommons.org/licenses/by/4.0/ Remote Sensing; Volume 15; Issue 5; Pages: 1205 ice thickness Shirase Glacier altimeter Text 2023 ftmdpi https://doi.org/10.3390/rs15051205 2023-08-01T08:56:18Z This study presents the feasibility of estimating the ice thickness of the Shirase Glacier using the synthetic aperture interferometric radar altimeter (SIRAL) on board the CryoSat-2 and the interannual variation of the ice thickness of the Shirase Glacier in 2011–2020. The SIRAL data were converted to ice thickness by assuming hydrostatic equilibrium, and the results showed that the ice thickness decreased from the grounding line to the terminus of the glacier. Furthermore, the ice thickness decreased 30 km downstream from the grounding line of the glacier in 2012 and 2017, and decreased 55 km and 60 km downstream from the grounding line of the glacier at other times, which was attributed to the discharge of landfast ice and the retreat of the glacier terminus. When the flow of glacial ice can be reasonably approximated as an incompressible fluid, and the law of conservation of mass can be applied to the ice stream, the multiple of the velocity and the underlying ice thickness under a constant ice density can be shown to correspond to the equation of continuity. Consequently, this study revealed that the ice thickness decreases with accelerating flow velocity, which is coincident with past outflow events. Text Shirase Glacier MDPI Open Access Publishing Shirase Glacier ENVELOPE(39.000,39.000,-70.333,-70.333) Remote Sensing 15 5 1205
institution Open Polar
collection MDPI Open Access Publishing
op_collection_id ftmdpi
language English
topic ice thickness
Shirase Glacier
altimeter
spellingShingle ice thickness
Shirase Glacier
altimeter
Yurina Satake
Kazuki Nakamura
Temporal Variations in Ice Thickness of the Shirase Glacier Derived from Cryosat-2/SIRAL Data
topic_facet ice thickness
Shirase Glacier
altimeter
description This study presents the feasibility of estimating the ice thickness of the Shirase Glacier using the synthetic aperture interferometric radar altimeter (SIRAL) on board the CryoSat-2 and the interannual variation of the ice thickness of the Shirase Glacier in 2011–2020. The SIRAL data were converted to ice thickness by assuming hydrostatic equilibrium, and the results showed that the ice thickness decreased from the grounding line to the terminus of the glacier. Furthermore, the ice thickness decreased 30 km downstream from the grounding line of the glacier in 2012 and 2017, and decreased 55 km and 60 km downstream from the grounding line of the glacier at other times, which was attributed to the discharge of landfast ice and the retreat of the glacier terminus. When the flow of glacial ice can be reasonably approximated as an incompressible fluid, and the law of conservation of mass can be applied to the ice stream, the multiple of the velocity and the underlying ice thickness under a constant ice density can be shown to correspond to the equation of continuity. Consequently, this study revealed that the ice thickness decreases with accelerating flow velocity, which is coincident with past outflow events.
format Text
author Yurina Satake
Kazuki Nakamura
author_facet Yurina Satake
Kazuki Nakamura
author_sort Yurina Satake
title Temporal Variations in Ice Thickness of the Shirase Glacier Derived from Cryosat-2/SIRAL Data
title_short Temporal Variations in Ice Thickness of the Shirase Glacier Derived from Cryosat-2/SIRAL Data
title_full Temporal Variations in Ice Thickness of the Shirase Glacier Derived from Cryosat-2/SIRAL Data
title_fullStr Temporal Variations in Ice Thickness of the Shirase Glacier Derived from Cryosat-2/SIRAL Data
title_full_unstemmed Temporal Variations in Ice Thickness of the Shirase Glacier Derived from Cryosat-2/SIRAL Data
title_sort temporal variations in ice thickness of the shirase glacier derived from cryosat-2/siral data
publisher Multidisciplinary Digital Publishing Institute
publishDate 2023
url https://doi.org/10.3390/rs15051205
op_coverage agris
long_lat ENVELOPE(39.000,39.000,-70.333,-70.333)
geographic Shirase Glacier
geographic_facet Shirase Glacier
genre Shirase Glacier
genre_facet Shirase Glacier
op_source Remote Sensing; Volume 15; Issue 5; Pages: 1205
op_relation Biogeosciences Remote Sensing
https://dx.doi.org/10.3390/rs15051205
op_rights https://creativecommons.org/licenses/by/4.0/
op_doi https://doi.org/10.3390/rs15051205
container_title Remote Sensing
container_volume 15
container_issue 5
container_start_page 1205
_version_ 1774723468732923904