CLOUD-RADIATIVE FORCING OVER THE SNOW-COVERED SURFACE AROUND ASUKA STATION, ANTARCTICA
Cloud-radiative forcing at the snow-covered surface in Antarctica was estimated from data of the radiation budget observation at Asuka Station (71°31'S, 24°08'E, 930m) in 1988. Cloud-radiative forcing at the top of the atmosphere was also estimated from satellite data in December 1988. It...
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Meteorological Research Institute
1992
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ftnipr:oai:nipr.repo.nii.ac.jp:00003700 2023-05-15T13:49:01+02:00 CLOUD-RADIATIVE FORCING OVER THE SNOW-COVERED SURFACE AROUND ASUKA STATION, ANTARCTICA アオキ テルオ ヤマノウチ タカシ Teruo AOKI Takashi YAMANOUCHI 1992-02 https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=3700 http://id.nii.ac.jp/1291/00003700/ https://nipr.repo.nii.ac.jp/?action=repository_action_common_download&item_id=3700&item_no=1&attribute_id=18&file_no=1 en eng Meteorological Research Institute National Institute of Polar Research https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=3700 http://id.nii.ac.jp/1291/00003700/ AA10756213 Proceedings of the NIPR Symposium on Polar Meteorology and Glaciology, 5, 76-89(1992-02) https://nipr.repo.nii.ac.jp/?action=repository_action_common_download&item_id=3700&item_no=1&attribute_id=18&file_no=1 Departmental Bulletin Paper P(論文) 1992 ftnipr 2022-12-10T19:45:46Z Cloud-radiative forcing at the snow-covered surface in Antarctica was estimated from data of the radiation budget observation at Asuka Station (71°31'S, 24°08'E, 930m) in 1988. Cloud-radiative forcing at the top of the atmosphere was also estimated from satellite data in December 1988. It was found that shortwave forcing was negative (cooling) at the surface and positive (heating) at the top of the atmosphere. The longwave forcing was positive both at the surface and at the top of the atmosphere. The (shortwave+longwave) forcing was positive both at the surface and at the top of the atmosphere. This is different from those in middle and the low latitudes. The cloud-radiative forcing distributions at the top of the atmosphere in the extended region from the sea to inland were estimated from the satellite data in December 1988. The results indicated that the shortwave forcing was positive over the snow-covered region except the high inland, and negative over the sea. The longwave forcing was positive over all regions. The (shortwave+longwave) forcing was positive over the snow-covered regions except the high inland plateau, and negative over the sea. Report Antarc* Antarctica Polar meteorology and glaciology Proceedings of the NIPR Symposium on Polar Meteorology and Glaciology National Institute of Polar Research Repository, Japan |
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Open Polar |
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National Institute of Polar Research Repository, Japan |
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ftnipr |
language |
English |
description |
Cloud-radiative forcing at the snow-covered surface in Antarctica was estimated from data of the radiation budget observation at Asuka Station (71°31'S, 24°08'E, 930m) in 1988. Cloud-radiative forcing at the top of the atmosphere was also estimated from satellite data in December 1988. It was found that shortwave forcing was negative (cooling) at the surface and positive (heating) at the top of the atmosphere. The longwave forcing was positive both at the surface and at the top of the atmosphere. The (shortwave+longwave) forcing was positive both at the surface and at the top of the atmosphere. This is different from those in middle and the low latitudes. The cloud-radiative forcing distributions at the top of the atmosphere in the extended region from the sea to inland were estimated from the satellite data in December 1988. The results indicated that the shortwave forcing was positive over the snow-covered region except the high inland, and negative over the sea. The longwave forcing was positive over all regions. The (shortwave+longwave) forcing was positive over the snow-covered regions except the high inland plateau, and negative over the sea. |
format |
Report |
author |
アオキ テルオ ヤマノウチ タカシ Teruo AOKI Takashi YAMANOUCHI |
spellingShingle |
アオキ テルオ ヤマノウチ タカシ Teruo AOKI Takashi YAMANOUCHI CLOUD-RADIATIVE FORCING OVER THE SNOW-COVERED SURFACE AROUND ASUKA STATION, ANTARCTICA |
author_facet |
アオキ テルオ ヤマノウチ タカシ Teruo AOKI Takashi YAMANOUCHI |
author_sort |
アオキ テルオ |
title |
CLOUD-RADIATIVE FORCING OVER THE SNOW-COVERED SURFACE AROUND ASUKA STATION, ANTARCTICA |
title_short |
CLOUD-RADIATIVE FORCING OVER THE SNOW-COVERED SURFACE AROUND ASUKA STATION, ANTARCTICA |
title_full |
CLOUD-RADIATIVE FORCING OVER THE SNOW-COVERED SURFACE AROUND ASUKA STATION, ANTARCTICA |
title_fullStr |
CLOUD-RADIATIVE FORCING OVER THE SNOW-COVERED SURFACE AROUND ASUKA STATION, ANTARCTICA |
title_full_unstemmed |
CLOUD-RADIATIVE FORCING OVER THE SNOW-COVERED SURFACE AROUND ASUKA STATION, ANTARCTICA |
title_sort |
cloud-radiative forcing over the snow-covered surface around asuka station, antarctica |
publisher |
Meteorological Research Institute |
publishDate |
1992 |
url |
https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=3700 http://id.nii.ac.jp/1291/00003700/ https://nipr.repo.nii.ac.jp/?action=repository_action_common_download&item_id=3700&item_no=1&attribute_id=18&file_no=1 |
genre |
Antarc* Antarctica Polar meteorology and glaciology Proceedings of the NIPR Symposium on Polar Meteorology and Glaciology |
genre_facet |
Antarc* Antarctica 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=3700 http://id.nii.ac.jp/1291/00003700/ AA10756213 Proceedings of the NIPR Symposium on Polar Meteorology and Glaciology, 5, 76-89(1992-02) https://nipr.repo.nii.ac.jp/?action=repository_action_common_download&item_id=3700&item_no=1&attribute_id=18&file_no=1 |
_version_ |
1766250421880356864 |