A probing radar designed for simulation of radar echo of a meteorite within the ice sheet of the Antarctic Continent (III) (abstract)

P(論文) We have succeeded in the simulation of a probing radar echo from meteorites within the ice sheet of the Antarctic Continent, and obtained the following. 1) On the region for the changing density profile, we did not obtain the probing radar echo from meteorites within the ice sheet. 2) As the p...

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Main Authors: Hoshiyama, Mitsuo, Nishitsuji, Akira, Nishio, Fumihiko, Wada, Makoto, Watanabe, Okitsugu
Language:English
Published: National Institute of Polar Research 1989
Subjects:
Online Access:https://nipr.repo.nii.ac.jp/record/3591/files/KJ00000035557.pdf
https://doi.org/10.15094/00003591
https://nipr.repo.nii.ac.jp/records/3591
_version_ 1829307549716840448
author Hoshiyama, Mitsuo
Nishitsuji, Akira
Nishio, Fumihiko
Wada, Makoto
Watanabe, Okitsugu
author_facet Hoshiyama, Mitsuo
Nishitsuji, Akira
Nishio, Fumihiko
Wada, Makoto
Watanabe, Okitsugu
author_sort Hoshiyama, Mitsuo
collection National Institute of Polar Research Repository, Japan
description P(論文) We have succeeded in the simulation of a probing radar echo from meteorites within the ice sheet of the Antarctic Continent, and obtained the following. 1) On the region for the changing density profile, we did not obtain the probing radar echo from meteorites within the ice sheet. 2) As the probing radar echoes are changed by the meteorite size, we had extreme difficulty in selecting the most useful frequency for the investigation of meteorites. So, when the equivalent radii of meteorites are selected to be 1,10,and 25 (cm), we have simulated to the radar echo from meteorites within the ice sheet. But, as radar echoes from meteorites there are often masked by echo signals from within the ice sheet, we have found the conditions that we can be detected the echo signals from meteorites. 3) When we have estimated for the number and radii of meteorites within the ice sheet, if can be observed by multitude radar frequencies, we can be estimated for it by the analysis of radar echoes. departmental bulletin paper
genre Antarc*
Antarctic
Ice Sheet
Polar meteorology and glaciology
Proceedings of the NIPR Symposium on Polar Meteorology and Glaciology
genre_facet Antarc*
Antarctic
Ice Sheet
Polar meteorology and glaciology
Proceedings of the NIPR Symposium on Polar Meteorology and Glaciology
geographic Antarctic
The Antarctic
geographic_facet Antarctic
The Antarctic
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institution Open Polar
language English
op_collection_id ftnipr
op_doi https://doi.org/10.15094/00003591
op_relation Proceedings of the NIPR Symposium on Polar Meteorology and Glaciology
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177
AA10756213
https://nipr.repo.nii.ac.jp/record/3591/files/KJ00000035557.pdf
https://doi.org/10.15094/00003591
https://nipr.repo.nii.ac.jp/records/3591
publishDate 1989
publisher National Institute of Polar Research
record_format openpolar
spelling ftnipr:oai:nipr.repo.nii.ac.jp:00003591 2025-04-13T14:07:36+00:00 A probing radar designed for simulation of radar echo of a meteorite within the ice sheet of the Antarctic Continent (III) (abstract) Hoshiyama, Mitsuo Nishitsuji, Akira Nishio, Fumihiko Wada, Makoto Watanabe, Okitsugu 1989-08 application/pdf https://nipr.repo.nii.ac.jp/record/3591/files/KJ00000035557.pdf https://doi.org/10.15094/00003591 https://nipr.repo.nii.ac.jp/records/3591 eng eng National Institute of Polar Research Proceedings of the NIPR Symposium on Polar Meteorology and Glaciology 2 177 AA10756213 https://nipr.repo.nii.ac.jp/record/3591/files/KJ00000035557.pdf https://doi.org/10.15094/00003591 https://nipr.repo.nii.ac.jp/records/3591 1989 ftnipr https://doi.org/10.15094/00003591 2025-03-19T10:19:56Z P(論文) We have succeeded in the simulation of a probing radar echo from meteorites within the ice sheet of the Antarctic Continent, and obtained the following. 1) On the region for the changing density profile, we did not obtain the probing radar echo from meteorites within the ice sheet. 2) As the probing radar echoes are changed by the meteorite size, we had extreme difficulty in selecting the most useful frequency for the investigation of meteorites. So, when the equivalent radii of meteorites are selected to be 1,10,and 25 (cm), we have simulated to the radar echo from meteorites within the ice sheet. But, as radar echoes from meteorites there are often masked by echo signals from within the ice sheet, we have found the conditions that we can be detected the echo signals from meteorites. 3) When we have estimated for the number and radii of meteorites within the ice sheet, if can be observed by multitude radar frequencies, we can be estimated for it by the analysis of radar echoes. departmental bulletin paper Other/Unknown Material Antarc* Antarctic Ice Sheet Polar meteorology and glaciology Proceedings of the NIPR Symposium on Polar Meteorology and Glaciology National Institute of Polar Research Repository, Japan Antarctic The Antarctic
spellingShingle Hoshiyama, Mitsuo
Nishitsuji, Akira
Nishio, Fumihiko
Wada, Makoto
Watanabe, Okitsugu
A probing radar designed for simulation of radar echo of a meteorite within the ice sheet of the Antarctic Continent (III) (abstract)
title A probing radar designed for simulation of radar echo of a meteorite within the ice sheet of the Antarctic Continent (III) (abstract)
title_full A probing radar designed for simulation of radar echo of a meteorite within the ice sheet of the Antarctic Continent (III) (abstract)
title_fullStr A probing radar designed for simulation of radar echo of a meteorite within the ice sheet of the Antarctic Continent (III) (abstract)
title_full_unstemmed A probing radar designed for simulation of radar echo of a meteorite within the ice sheet of the Antarctic Continent (III) (abstract)
title_short A probing radar designed for simulation of radar echo of a meteorite within the ice sheet of the Antarctic Continent (III) (abstract)
title_sort probing radar designed for simulation of radar echo of a meteorite within the ice sheet of the antarctic continent (iii) (abstract)
url https://nipr.repo.nii.ac.jp/record/3591/files/KJ00000035557.pdf
https://doi.org/10.15094/00003591
https://nipr.repo.nii.ac.jp/records/3591