Radio echo sounding in the area of the Yamato Mountains
P(論文) In the bare ice area of the Yamato Mountains about 4000 pieces of meteorite were found by the Japanese Antarctic Research Expedition (JARE). The most plausible explanation of the mechanism of meteorite concentration in the area was presented by NAGATA. In order to survey the bedrock topography...
Main Authors: | , , , |
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Language: | English |
Published: |
1981
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Online Access: | https://nipr.repo.nii.ac.jp/record/1199/files/KJ00000011725.pdf https://nipr.repo.nii.ac.jp/records/1199 |
_version_ | 1829302070091448320 |
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author | Wada, Makoto Yamanouchi, Takashi Mae, Shinji Kusunoki, Kou |
author_facet | Wada, Makoto Yamanouchi, Takashi Mae, Shinji Kusunoki, Kou |
author_sort | Wada, Makoto |
collection | National Institute of Polar Research Repository, Japan |
description | P(論文) In the bare ice area of the Yamato Mountains about 4000 pieces of meteorite were found by the Japanese Antarctic Research Expedition (JARE). The most plausible explanation of the mechanism of meteorite concentration in the area was presented by NAGATA. In order to survey the bedrock topography in the bare ice area airborne radio echo sounding was carried out in January 1980. The new sounder (NIPR-A) was operated at 179 MHz and mounted in a Pilatus Poter PC-6. The peak power of the sounder was approximately 1kW and the pulse width was 0.3μs. The line of the survey consisted of 5 parts, each being 80km long. Two of them were parallel to the north-south direction and three were parallel to the east-west direction. Their interval was about 30km. In this paper, the result of the survey on the topography of the bedrock and the surface is reported and especially the ice flow near Motoi Nunatak where the flow velocity and the ablation rate of ice were measured is commented. The bare ice area where a lot of meteorites were found is a flat surface area upstream of subsurface mountains. departmental bulletin paper |
genre | Antarc* Antarctic Memoirs of National Institute of Polar Research Polar Research |
genre_facet | Antarc* Antarctic Memoirs of National Institute of Polar Research Polar Research |
geographic | Antarctic Yamato Nagata Pilatus |
geographic_facet | Antarctic Yamato Nagata Pilatus |
id | ftnipr:oai:nipr.repo.nii.ac.jp:00001199 |
institution | Open Polar |
language | English |
long_lat | ENVELOPE(35.583,35.583,-71.417,-71.417) ENVELOPE(162.783,162.783,-71.350,-71.350) ENVELOPE(15.249,15.249,68.755,68.755) |
op_collection_id | ftnipr |
op_relation | Memoirs of National Institute of Polar Research. Special issue 20 17 24 AA00733561 https://nipr.repo.nii.ac.jp/record/1199/files/KJ00000011725.pdf https://nipr.repo.nii.ac.jp/records/1199 |
publishDate | 1981 |
record_format | openpolar |
spelling | ftnipr:oai:nipr.repo.nii.ac.jp:00001199 2025-04-13T14:10:16+00:00 Radio echo sounding in the area of the Yamato Mountains Wada, Makoto Yamanouchi, Takashi Mae, Shinji Kusunoki, Kou 1981-12 application/pdf https://nipr.repo.nii.ac.jp/record/1199/files/KJ00000011725.pdf https://nipr.repo.nii.ac.jp/records/1199 eng eng Memoirs of National Institute of Polar Research. Special issue 20 17 24 AA00733561 https://nipr.repo.nii.ac.jp/record/1199/files/KJ00000011725.pdf https://nipr.repo.nii.ac.jp/records/1199 1981 ftnipr 2025-03-19T10:19:57Z P(論文) In the bare ice area of the Yamato Mountains about 4000 pieces of meteorite were found by the Japanese Antarctic Research Expedition (JARE). The most plausible explanation of the mechanism of meteorite concentration in the area was presented by NAGATA. In order to survey the bedrock topography in the bare ice area airborne radio echo sounding was carried out in January 1980. The new sounder (NIPR-A) was operated at 179 MHz and mounted in a Pilatus Poter PC-6. The peak power of the sounder was approximately 1kW and the pulse width was 0.3μs. The line of the survey consisted of 5 parts, each being 80km long. Two of them were parallel to the north-south direction and three were parallel to the east-west direction. Their interval was about 30km. In this paper, the result of the survey on the topography of the bedrock and the surface is reported and especially the ice flow near Motoi Nunatak where the flow velocity and the ablation rate of ice were measured is commented. The bare ice area where a lot of meteorites were found is a flat surface area upstream of subsurface mountains. departmental bulletin paper Other/Unknown Material Antarc* Antarctic Memoirs of National Institute of Polar Research Polar Research National Institute of Polar Research Repository, Japan Antarctic Yamato ENVELOPE(35.583,35.583,-71.417,-71.417) Nagata ENVELOPE(162.783,162.783,-71.350,-71.350) Pilatus ENVELOPE(15.249,15.249,68.755,68.755) |
spellingShingle | Wada, Makoto Yamanouchi, Takashi Mae, Shinji Kusunoki, Kou Radio echo sounding in the area of the Yamato Mountains |
title | Radio echo sounding in the area of the Yamato Mountains |
title_full | Radio echo sounding in the area of the Yamato Mountains |
title_fullStr | Radio echo sounding in the area of the Yamato Mountains |
title_full_unstemmed | Radio echo sounding in the area of the Yamato Mountains |
title_short | Radio echo sounding in the area of the Yamato Mountains |
title_sort | radio echo sounding in the area of the yamato mountains |
url | https://nipr.repo.nii.ac.jp/record/1199/files/KJ00000011725.pdf https://nipr.repo.nii.ac.jp/records/1199 |