INFLUENCES OF ARCTIC OZONE HOLE ON THE STRATOSPHERIC GENERAL CIRCULATION
P(論文) Numerical experiments are performed for four years to estimate radiative and dynamical influences of the "Arctic ozone hole" on the stratospheric general circulation by using a general circulation model developed at Kyushu University. The model includes simplified ozone photochemistr...
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Language: | English |
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National Institute of Polar Research
1999
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Online Access: | https://nipr.repo.nii.ac.jp/record/2884/files/KJ00002409899.pdf https://doi.org/10.15094/00002884 https://nipr.repo.nii.ac.jp/records/2884 |
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author | ヒロオカ, トシヒコ ニシヨシ, トシヒコ ワタナベ, シンゴ ミヤハラ, サブロウ HIROOKA, Toshihiko NISHIYOSHI, Toshihiko WATANABE, Shingo MIYAHARA, Saburo |
author_facet | ヒロオカ, トシヒコ ニシヨシ, トシヒコ ワタナベ, シンゴ ミヤハラ, サブロウ HIROOKA, Toshihiko NISHIYOSHI, Toshihiko WATANABE, Shingo MIYAHARA, Saburo |
author_sort | ヒロオカ, トシヒコ |
collection | National Institute of Polar Research Repository, Japan |
description | P(論文) Numerical experiments are performed for four years to estimate radiative and dynamical influences of the "Arctic ozone hole" on the stratospheric general circulation by using a general circulation model developed at Kyushu University. The model includes simplified ozone photochemistry interactively coupled with radiation and dynamics. The resultant temperature structure consists of cooling of about 6K in the polar lower stratosphere and warming of about 8K in the polar upper stratosphere, which intensifies the polar night jet by about 9ms^<-1>. The cooling is caused by reduction of downward motion as well as decrease of solar UV heating due to ozone depletion, while the warming is caused by dynamical heating due to enhancement of downward motion. The results imply that the feedback mechanism may strengthen the ozone hole itself. departmental bulletin paper |
genre | Arctic Polar meteorology and glaciology polar night |
genre_facet | Arctic Polar meteorology and glaciology polar night |
geographic | Arctic |
geographic_facet | Arctic |
id | ftnipr:oai:nipr.repo.nii.ac.jp:00002884 |
institution | Open Polar |
language | English |
op_collection_id | ftnipr |
op_doi | https://doi.org/10.15094/00002884 |
op_relation | Polar meteorology and glaciology 13 1 10 AA1129795X https://nipr.repo.nii.ac.jp/record/2884/files/KJ00002409899.pdf https://doi.org/10.15094/00002884 https://nipr.repo.nii.ac.jp/records/2884 |
publishDate | 1999 |
publisher | National Institute of Polar Research |
record_format | openpolar |
spelling | ftnipr:oai:nipr.repo.nii.ac.jp:00002884 2025-04-13T14:13:42+00:00 INFLUENCES OF ARCTIC OZONE HOLE ON THE STRATOSPHERIC GENERAL CIRCULATION ヒロオカ, トシヒコ ニシヨシ, トシヒコ ワタナベ, シンゴ ミヤハラ, サブロウ HIROOKA, Toshihiko NISHIYOSHI, Toshihiko WATANABE, Shingo MIYAHARA, Saburo 1999-12 application/pdf https://nipr.repo.nii.ac.jp/record/2884/files/KJ00002409899.pdf https://doi.org/10.15094/00002884 https://nipr.repo.nii.ac.jp/records/2884 eng eng National Institute of Polar Research Polar meteorology and glaciology 13 1 10 AA1129795X https://nipr.repo.nii.ac.jp/record/2884/files/KJ00002409899.pdf https://doi.org/10.15094/00002884 https://nipr.repo.nii.ac.jp/records/2884 1999 ftnipr https://doi.org/10.15094/00002884 2025-03-19T10:19:56Z P(論文) Numerical experiments are performed for four years to estimate radiative and dynamical influences of the "Arctic ozone hole" on the stratospheric general circulation by using a general circulation model developed at Kyushu University. The model includes simplified ozone photochemistry interactively coupled with radiation and dynamics. The resultant temperature structure consists of cooling of about 6K in the polar lower stratosphere and warming of about 8K in the polar upper stratosphere, which intensifies the polar night jet by about 9ms^<-1>. The cooling is caused by reduction of downward motion as well as decrease of solar UV heating due to ozone depletion, while the warming is caused by dynamical heating due to enhancement of downward motion. The results imply that the feedback mechanism may strengthen the ozone hole itself. departmental bulletin paper Other/Unknown Material Arctic Polar meteorology and glaciology polar night National Institute of Polar Research Repository, Japan Arctic |
spellingShingle | ヒロオカ, トシヒコ ニシヨシ, トシヒコ ワタナベ, シンゴ ミヤハラ, サブロウ HIROOKA, Toshihiko NISHIYOSHI, Toshihiko WATANABE, Shingo MIYAHARA, Saburo INFLUENCES OF ARCTIC OZONE HOLE ON THE STRATOSPHERIC GENERAL CIRCULATION |
title | INFLUENCES OF ARCTIC OZONE HOLE ON THE STRATOSPHERIC GENERAL CIRCULATION |
title_full | INFLUENCES OF ARCTIC OZONE HOLE ON THE STRATOSPHERIC GENERAL CIRCULATION |
title_fullStr | INFLUENCES OF ARCTIC OZONE HOLE ON THE STRATOSPHERIC GENERAL CIRCULATION |
title_full_unstemmed | INFLUENCES OF ARCTIC OZONE HOLE ON THE STRATOSPHERIC GENERAL CIRCULATION |
title_short | INFLUENCES OF ARCTIC OZONE HOLE ON THE STRATOSPHERIC GENERAL CIRCULATION |
title_sort | influences of arctic ozone hole on the stratospheric general circulation |
url | https://nipr.repo.nii.ac.jp/record/2884/files/KJ00002409899.pdf https://doi.org/10.15094/00002884 https://nipr.repo.nii.ac.jp/records/2884 |