CHARACTERISTICS OF RADIO ATTENUATION COEFFICIENT ON THE SØR RONDARNE ICE SHEET, ANTARCTICA
The depth-averaged attenuation coefficients are calculated from the echo pattern measurements from internal ice. The attenuation coefficients around the Sør Rondane Mountains, Antarctica were mapped from the 179MHz airborne radio-echo sounder, which made observations during 1986. The map shows a ten...
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ftnipr:oai:nipr.repo.nii.ac.jp:00003997 2023-05-15T13:49:01+02:00 CHARACTERISTICS OF RADIO ATTENUATION COEFFICIENT ON THE SØR RONDARNE ICE SHEET, ANTARCTICA マエノ ヒデオ ウラツカ セイホ Hideo MAENO Seiho URATSUKA 1997-11 https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=3997 http://id.nii.ac.jp/1291/00003997/ https://nipr.repo.nii.ac.jp/?action=repository_action_common_download&item_id=3997&item_no=1&attribute_id=18&file_no=1 en eng ABSTRACT Communications Research Laboratory, Ministry of Posts and Telecommunications National Institute of Polar Research https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=3997 http://id.nii.ac.jp/1291/00003997/ AA10756213 Proceedings of the NIPR Symposium on Polar Meteorology and Glaciology, 11, 252(1997-11) https://nipr.repo.nii.ac.jp/?action=repository_action_common_download&item_id=3997&item_no=1&attribute_id=18&file_no=1 Departmental Bulletin Paper P(論文) 1997 ftnipr 2023-01-14T19:56:31Z The depth-averaged attenuation coefficients are calculated from the echo pattern measurements from internal ice. The attenuation coefficients around the Sør Rondane Mountains, Antarctica were mapped from the 179MHz airborne radio-echo sounder, which made observations during 1986. The map shows a tendency of decreasing attenuation as the surface altitude of the ice sheet increases. This result is interpreted by using the relationship between attenuation coefficients and ice temperature. In addition, a cosine relationship was found between attenuation coefficients and the angle of the radar polarization from the topographic contour. The dynamic range of the variety of the attenuation coefficients is 1.2dB/100m. If the ice flow is perpendicular to the topographic contour, the ice flow direction will be derived from the polarimetric radar observation. Report Antarc* Antarctica Ice Sheet Polar meteorology and glaciology Proceedings of the NIPR Symposium on Polar Meteorology and Glaciology National Institute of Polar Research Repository, Japan Sør Rondane Mountains ENVELOPE(25.000,25.000,-72.000,-72.000) Sør-Rondane ENVELOPE(25.000,25.000,-72.000,-72.000) |
institution |
Open Polar |
collection |
National Institute of Polar Research Repository, Japan |
op_collection_id |
ftnipr |
language |
English |
description |
The depth-averaged attenuation coefficients are calculated from the echo pattern measurements from internal ice. The attenuation coefficients around the Sør Rondane Mountains, Antarctica were mapped from the 179MHz airborne radio-echo sounder, which made observations during 1986. The map shows a tendency of decreasing attenuation as the surface altitude of the ice sheet increases. This result is interpreted by using the relationship between attenuation coefficients and ice temperature. In addition, a cosine relationship was found between attenuation coefficients and the angle of the radar polarization from the topographic contour. The dynamic range of the variety of the attenuation coefficients is 1.2dB/100m. If the ice flow is perpendicular to the topographic contour, the ice flow direction will be derived from the polarimetric radar observation. |
format |
Report |
author |
マエノ ヒデオ ウラツカ セイホ Hideo MAENO Seiho URATSUKA |
spellingShingle |
マエノ ヒデオ ウラツカ セイホ Hideo MAENO Seiho URATSUKA CHARACTERISTICS OF RADIO ATTENUATION COEFFICIENT ON THE SØR RONDARNE ICE SHEET, ANTARCTICA |
author_facet |
マエノ ヒデオ ウラツカ セイホ Hideo MAENO Seiho URATSUKA |
author_sort |
マエノ ヒデオ |
title |
CHARACTERISTICS OF RADIO ATTENUATION COEFFICIENT ON THE SØR RONDARNE ICE SHEET, ANTARCTICA |
title_short |
CHARACTERISTICS OF RADIO ATTENUATION COEFFICIENT ON THE SØR RONDARNE ICE SHEET, ANTARCTICA |
title_full |
CHARACTERISTICS OF RADIO ATTENUATION COEFFICIENT ON THE SØR RONDARNE ICE SHEET, ANTARCTICA |
title_fullStr |
CHARACTERISTICS OF RADIO ATTENUATION COEFFICIENT ON THE SØR RONDARNE ICE SHEET, ANTARCTICA |
title_full_unstemmed |
CHARACTERISTICS OF RADIO ATTENUATION COEFFICIENT ON THE SØR RONDARNE ICE SHEET, ANTARCTICA |
title_sort |
characteristics of radio attenuation coefficient on the sør rondarne ice sheet, antarctica |
publisher |
ABSTRACT |
publishDate |
1997 |
url |
https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=3997 http://id.nii.ac.jp/1291/00003997/ https://nipr.repo.nii.ac.jp/?action=repository_action_common_download&item_id=3997&item_no=1&attribute_id=18&file_no=1 |
long_lat |
ENVELOPE(25.000,25.000,-72.000,-72.000) ENVELOPE(25.000,25.000,-72.000,-72.000) |
geographic |
Sør Rondane Mountains Sør-Rondane |
geographic_facet |
Sør Rondane Mountains Sør-Rondane |
genre |
Antarc* Antarctica Ice Sheet Polar meteorology and glaciology Proceedings of the NIPR Symposium on Polar Meteorology and Glaciology |
genre_facet |
Antarc* Antarctica Ice Sheet Polar meteorology and glaciology Proceedings of the NIPR Symposium on Polar Meteorology and Glaciology |
op_relation |
https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=3997 http://id.nii.ac.jp/1291/00003997/ AA10756213 Proceedings of the NIPR Symposium on Polar Meteorology and Glaciology, 11, 252(1997-11) https://nipr.repo.nii.ac.jp/?action=repository_action_common_download&item_id=3997&item_no=1&attribute_id=18&file_no=1 |
_version_ |
1766250454188032000 |