Time series of basal melt rates of the Roi Baudouin Ice Shelf, Antarctica

Ice shelves play a crucial role in helping controlling the current rate of mass loss from the Antarctic ice sheet through their buttressing potential. This control is modulated by variations in ice shelf mass balance, which cause changes in the thickness of the ice shelf, and therefore in its abilit...

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Main Authors: Sun, Sainan, Hattermann, Tore, Pattyn, Frank, Drews, Reinhard, Berger, Sophie
Format: Article in Journal/Newspaper
Language:English
Published: PANGAEA - Data Publisher for Earth & Environmental Science 2019
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.903182
https://doi.pangaea.de/10.1594/PANGAEA.903182
id ftdatacite:10.1594/pangaea.903182
record_format openpolar
spelling ftdatacite:10.1594/pangaea.903182 2023-05-15T14:05:25+02:00 Time series of basal melt rates of the Roi Baudouin Ice Shelf, Antarctica Sun, Sainan Hattermann, Tore Pattyn, Frank Drews, Reinhard Berger, Sophie 2019 application/zip https://dx.doi.org/10.1594/pangaea.903182 https://doi.pangaea.de/10.1594/PANGAEA.903182 en eng PANGAEA - Data Publisher for Earth & Environmental Science https://dx.doi.org/10.1029/2019gl083881 Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 CC-BY 1 year time series ApRES basal ice shelf melt rates ice-ocean interaction Multiple investigations Collection of Datasets article Collection 2019 ftdatacite https://doi.org/10.1594/pangaea.903182 https://doi.org/10.1029/2019gl083881 2022-02-09T13:17:41Z Ice shelves play a crucial role in helping controlling the current rate of mass loss from the Antarctic ice sheet through their buttressing potential. This control is modulated by variations in ice shelf mass balance, which cause changes in the thickness of the ice shelf, and therefore in its ability to restrain flow from the grounded ice sheet. We present results showing temporal variability in sub-shelf melting using autonomous phase-sensitive radio-echo sounders (ApRES) near the grounding line of the Roi Baudouin Ice Shelf, Dronning Maud Land, East Antarctica. When combined with additional oceanographic evidence of seasonal variation in stratification and the amplification of the diurnal tides around the Gunnerus Bank, the results suggest an intricate mechanism in which topographic waves control the seasonal melt rate variability near the grounding line of the Roi Baudouin Ice Shelf. Article in Journal/Newspaper Antarc* Antarctic Antarctica Dronning Maud Land East Antarctica Ice Sheet Ice Shelf Ice Shelves DataCite Metadata Store (German National Library of Science and Technology) Antarctic The Antarctic East Antarctica Dronning Maud Land Roi Baudouin ENVELOPE(24.461,24.461,-70.438,-70.438) Gunnerus Bank ENVELOPE(33.000,33.000,-68.000,-68.000)
institution Open Polar
collection DataCite Metadata Store (German National Library of Science and Technology)
op_collection_id ftdatacite
language English
topic 1 year time series
ApRES
basal ice shelf melt rates
ice-ocean interaction
Multiple investigations
spellingShingle 1 year time series
ApRES
basal ice shelf melt rates
ice-ocean interaction
Multiple investigations
Sun, Sainan
Hattermann, Tore
Pattyn, Frank
Drews, Reinhard
Berger, Sophie
Time series of basal melt rates of the Roi Baudouin Ice Shelf, Antarctica
topic_facet 1 year time series
ApRES
basal ice shelf melt rates
ice-ocean interaction
Multiple investigations
description Ice shelves play a crucial role in helping controlling the current rate of mass loss from the Antarctic ice sheet through their buttressing potential. This control is modulated by variations in ice shelf mass balance, which cause changes in the thickness of the ice shelf, and therefore in its ability to restrain flow from the grounded ice sheet. We present results showing temporal variability in sub-shelf melting using autonomous phase-sensitive radio-echo sounders (ApRES) near the grounding line of the Roi Baudouin Ice Shelf, Dronning Maud Land, East Antarctica. When combined with additional oceanographic evidence of seasonal variation in stratification and the amplification of the diurnal tides around the Gunnerus Bank, the results suggest an intricate mechanism in which topographic waves control the seasonal melt rate variability near the grounding line of the Roi Baudouin Ice Shelf.
format Article in Journal/Newspaper
author Sun, Sainan
Hattermann, Tore
Pattyn, Frank
Drews, Reinhard
Berger, Sophie
author_facet Sun, Sainan
Hattermann, Tore
Pattyn, Frank
Drews, Reinhard
Berger, Sophie
author_sort Sun, Sainan
title Time series of basal melt rates of the Roi Baudouin Ice Shelf, Antarctica
title_short Time series of basal melt rates of the Roi Baudouin Ice Shelf, Antarctica
title_full Time series of basal melt rates of the Roi Baudouin Ice Shelf, Antarctica
title_fullStr Time series of basal melt rates of the Roi Baudouin Ice Shelf, Antarctica
title_full_unstemmed Time series of basal melt rates of the Roi Baudouin Ice Shelf, Antarctica
title_sort time series of basal melt rates of the roi baudouin ice shelf, antarctica
publisher PANGAEA - Data Publisher for Earth & Environmental Science
publishDate 2019
url https://dx.doi.org/10.1594/pangaea.903182
https://doi.pangaea.de/10.1594/PANGAEA.903182
long_lat ENVELOPE(24.461,24.461,-70.438,-70.438)
ENVELOPE(33.000,33.000,-68.000,-68.000)
geographic Antarctic
The Antarctic
East Antarctica
Dronning Maud Land
Roi Baudouin
Gunnerus Bank
geographic_facet Antarctic
The Antarctic
East Antarctica
Dronning Maud Land
Roi Baudouin
Gunnerus Bank
genre Antarc*
Antarctic
Antarctica
Dronning Maud Land
East Antarctica
Ice Sheet
Ice Shelf
Ice Shelves
genre_facet Antarc*
Antarctic
Antarctica
Dronning Maud Land
East Antarctica
Ice Sheet
Ice Shelf
Ice Shelves
op_relation https://dx.doi.org/10.1029/2019gl083881
op_rights Creative Commons Attribution 4.0 International
https://creativecommons.org/licenses/by/4.0/legalcode
cc-by-4.0
op_rightsnorm CC-BY
op_doi https://doi.org/10.1594/pangaea.903182
https://doi.org/10.1029/2019gl083881
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