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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National Institute of Polar Research
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ftdoajarticles:oai:doaj.org/article:48d1e9931db9476090e33acbacbd22ac 2023-05-15T13:39:48+02:00 Report on the geomorphological survey in the Soya Coast (JARE-61) Takeshige Ishiwa Yuki Tokuda Takuya Itaki Satoshi Sasaki 2020-11-01T00:00:00Z https://doi.org/10.15094/00016229 https://doaj.org/article/48d1e9931db9476090e33acbacbd22ac EN JA eng jpn National Institute of Polar Research https://doaj.org/toc/0085-7289 https://doaj.org/toc/2432-079X http://doi.org/10.15094/00016229 0085-7289 2432-079X https://doaj.org/article/48d1e9931db9476090e33acbacbd22ac Antarctic Record, Vol 64, Pp 330-350 (2020) antarctic ice sheet sea-level change lake marine and terrestrial sediments soya coast Geography (General) G1-922 article 2020 ftdoajarticles https://doi.org/10.15094/00016229 2022-12-31T15:07:30Z 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 Directory of Open Access Journals: DOAJ Articles Antarctic The Antarctic East Antarctica Ongul ENVELOPE(39.533,39.533,-69.017,-69.017) Ongul Island ENVELOPE(39.533,39.533,-69.017,-69.017) Langhovde ENVELOPE(39.733,39.733,-69.217,-69.217) Lützow-Holm Bay ENVELOPE(38.000,38.000,-69.500,-69.500) |
institution |
Open Polar |
collection |
Directory of Open Access Journals: DOAJ Articles |
op_collection_id |
ftdoajarticles |
language |
English Japanese |
topic |
antarctic ice sheet sea-level change lake marine and terrestrial sediments soya coast Geography (General) G1-922 |
spellingShingle |
antarctic ice sheet sea-level change lake marine and terrestrial sediments soya coast Geography (General) G1-922 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 Geography (General) G1-922 |
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 https://doaj.org/article/48d1e9931db9476090e33acbacbd22ac |
long_lat |
ENVELOPE(39.533,39.533,-69.017,-69.017) ENVELOPE(39.533,39.533,-69.017,-69.017) ENVELOPE(39.733,39.733,-69.217,-69.217) ENVELOPE(38.000,38.000,-69.500,-69.500) |
geographic |
Antarctic The Antarctic East Antarctica Ongul Ongul Island Langhovde Lützow-Holm Bay |
geographic_facet |
Antarctic The Antarctic East Antarctica Ongul Ongul Island Langhovde Lützow-Holm Bay |
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 |
https://doaj.org/toc/0085-7289 https://doaj.org/toc/2432-079X http://doi.org/10.15094/00016229 0085-7289 2432-079X https://doaj.org/article/48d1e9931db9476090e33acbacbd22ac |
op_doi |
https://doi.org/10.15094/00016229 |
_version_ |
1766124955305508864 |