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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Main Authors: 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
Language:English
Published: National Institute of Polar Research 1999
Subjects:
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
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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