Report on the geomorphological survey in the Soya Coast (JARE-61)

The Antarctic Ice Sheet is a major source of future sea-level rise due to global warming. Reconstruction of the past Antarctic Ice Sheet is essential to understand the mechanism of the Antarctic Ice Sheet response to global and regional climate changes. However, the shortage of geological evidence o...

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Main Authors: Takeshige Ishiwa, Yuki Tokuda, Takuya Itaki, Satoshi Sasaki
Format: Article in Journal/Newspaper
Language:English
Published: National Institute of Polar Research 2020
Subjects:
geo
Online Access:https://doi.org/10.15094/00016229
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spelling fttriple:oai:gotriple.eu:oai:doaj.org/article:48d1e9931db9476090e33acbacbd22ac 2023-05-15T14:00:43+02:00 Report on the geomorphological survey in the Soya Coast (JARE-61) Takeshige Ishiwa Yuki Tokuda Takuya Itaki Satoshi Sasaki 2020-11-01 https://doi.org/10.15094/00016229 en other eng National Institute of Polar Research 0085-7289 2432-079X http://doi.org/10.15094/00016229 undefined Antarctic Record, Vol 64, Pp 330-350 (2020) antarctic ice sheet sea-level change lake marine and terrestrial sediments soya coast geo envir Journal Article https://vocabularies.coar-repositories.org/resource_types/c_6501/ 2020 fttriple https://doi.org/10.15094/00016229 2023-01-22T17:58:07Z The Antarctic Ice Sheet is a major source of future sea-level rise due to global warming. Reconstruction of the past Antarctic Ice Sheet is essential to understand the mechanism of the Antarctic Ice Sheet response to global and regional climate changes. However, the shortage of geological evidence of sea-level and ice-sheet records makes it difficult to reconstruct the Antarctic Ice Sheet changes. The geomorphological survey is conducted in the 61st Japanese Research Antarctic Research Expedition, and the objective of this survey is to obtain sea-level and ice-sheet records from Lützow-Holm Bay in East Antarctica. We measured the bathymetry and collected sediment samples in shallow water of Langhovde. We also collected the rocks for measuring cosmogenic nuclide and the terrestrial surface sediments, and took an interference pattern under the ground by the ground-penetrating radar in both the Langhovde and West Ongul Island. The data collected will be used to obtain geological evidence of the Antarctic Ice Sheet changes in the future expedition. We report the summary of the geomorphological survey such as planning, logistics, and records. Article in Journal/Newspaper Antarc* Antarctic Antarctica East Antarctica Ice Sheet Ongul Island Unknown Antarctic East Antarctica Langhovde ENVELOPE(39.733,39.733,-69.217,-69.217) Lützow-Holm Bay ENVELOPE(38.000,38.000,-69.500,-69.500) Ongul ENVELOPE(39.533,39.533,-69.017,-69.017) Ongul Island ENVELOPE(39.533,39.533,-69.017,-69.017) The Antarctic
institution Open Polar
collection Unknown
op_collection_id fttriple
language English
topic antarctic ice sheet
sea-level change
lake
marine
and terrestrial sediments
soya coast
geo
envir
spellingShingle antarctic ice sheet
sea-level change
lake
marine
and terrestrial sediments
soya coast
geo
envir
Takeshige Ishiwa
Yuki Tokuda
Takuya Itaki
Satoshi Sasaki
Report on the geomorphological survey in the Soya Coast (JARE-61)
topic_facet antarctic ice sheet
sea-level change
lake
marine
and terrestrial sediments
soya coast
geo
envir
description The Antarctic Ice Sheet is a major source of future sea-level rise due to global warming. Reconstruction of the past Antarctic Ice Sheet is essential to understand the mechanism of the Antarctic Ice Sheet response to global and regional climate changes. However, the shortage of geological evidence of sea-level and ice-sheet records makes it difficult to reconstruct the Antarctic Ice Sheet changes. The geomorphological survey is conducted in the 61st Japanese Research Antarctic Research Expedition, and the objective of this survey is to obtain sea-level and ice-sheet records from Lützow-Holm Bay in East Antarctica. We measured the bathymetry and collected sediment samples in shallow water of Langhovde. We also collected the rocks for measuring cosmogenic nuclide and the terrestrial surface sediments, and took an interference pattern under the ground by the ground-penetrating radar in both the Langhovde and West Ongul Island. The data collected will be used to obtain geological evidence of the Antarctic Ice Sheet changes in the future expedition. We report the summary of the geomorphological survey such as planning, logistics, and records.
format Article in Journal/Newspaper
author Takeshige Ishiwa
Yuki Tokuda
Takuya Itaki
Satoshi Sasaki
author_facet Takeshige Ishiwa
Yuki Tokuda
Takuya Itaki
Satoshi Sasaki
author_sort Takeshige Ishiwa
title Report on the geomorphological survey in the Soya Coast (JARE-61)
title_short Report on the geomorphological survey in the Soya Coast (JARE-61)
title_full Report on the geomorphological survey in the Soya Coast (JARE-61)
title_fullStr Report on the geomorphological survey in the Soya Coast (JARE-61)
title_full_unstemmed Report on the geomorphological survey in the Soya Coast (JARE-61)
title_sort report on the geomorphological survey in the soya coast (jare-61)
publisher National Institute of Polar Research
publishDate 2020
url https://doi.org/10.15094/00016229
long_lat ENVELOPE(39.733,39.733,-69.217,-69.217)
ENVELOPE(38.000,38.000,-69.500,-69.500)
ENVELOPE(39.533,39.533,-69.017,-69.017)
ENVELOPE(39.533,39.533,-69.017,-69.017)
geographic Antarctic
East Antarctica
Langhovde
Lützow-Holm Bay
Ongul
Ongul Island
The Antarctic
geographic_facet Antarctic
East Antarctica
Langhovde
Lützow-Holm Bay
Ongul
Ongul Island
The Antarctic
genre Antarc*
Antarctic
Antarctica
East Antarctica
Ice Sheet
Ongul Island
genre_facet Antarc*
Antarctic
Antarctica
East Antarctica
Ice Sheet
Ongul Island
op_source Antarctic Record, Vol 64, Pp 330-350 (2020)
op_relation 0085-7289
2432-079X
http://doi.org/10.15094/00016229
op_rights undefined
op_doi https://doi.org/10.15094/00016229
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