MEAN-MERIDIONAL CIRCULATION OF THE POLAR STRATOSPHERE REPRODUCED IN A GCM

The lower-stratospheric circulation of a GCM is analyzed with the new TEM scheme in the pressure-isentrope hybrid vertical coordinate. The polar stratospheric downward mass flux in winter is found to be much larger in the NH than in the SH.

Bibliographic Details
Main Authors: イワサキ トシキ, Toshiki IWASAKI
Format: Report
Language:English
Published: Japan Meteorological Agency 1992
Subjects:
Polar meteorology and glaciology
Proceedings of the NIPR Symposium on Polar Meteorology and Glaciology
Online Access:https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=3695
http://id.nii.ac.jp/1291/00003695/
https://nipr.repo.nii.ac.jp/?action=repository_action_common_download&item_id=3695&item_no=1&attribute_id=18&file_no=1
id ftnipr:oai:nipr.repo.nii.ac.jp:00003695
record_format openpolar
spelling ftnipr:oai:nipr.repo.nii.ac.jp:00003695 2023-05-15T18:02:11+02:00 MEAN-MERIDIONAL CIRCULATION OF THE POLAR STRATOSPHERE REPRODUCED IN A GCM イワサキ トシキ Toshiki IWASAKI 1992-02 https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=3695 http://id.nii.ac.jp/1291/00003695/ https://nipr.repo.nii.ac.jp/?action=repository_action_common_download&item_id=3695&item_no=1&attribute_id=18&file_no=1 en eng Japan Meteorological Agency National Institute of Polar Research https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=3695 http://id.nii.ac.jp/1291/00003695/ AA10756213 Proceedings of the NIPR Symposium on Polar Meteorology and Glaciology, 5, 24-28(1992-02) https://nipr.repo.nii.ac.jp/?action=repository_action_common_download&item_id=3695&item_no=1&attribute_id=18&file_no=1 Departmental Bulletin Paper P(論文) 1992 ftnipr 2022-12-10T19:45:46Z The lower-stratospheric circulation of a GCM is analyzed with the new TEM scheme in the pressure-isentrope hybrid vertical coordinate. The polar stratospheric downward mass flux in winter is found to be much larger in the NH than in the SH. Report Polar meteorology and glaciology Proceedings of the NIPR Symposium on Polar Meteorology and Glaciology National Institute of Polar Research Repository, Japan
institution Open Polar
collection National Institute of Polar Research Repository, Japan
op_collection_id ftnipr
language English
description The lower-stratospheric circulation of a GCM is analyzed with the new TEM scheme in the pressure-isentrope hybrid vertical coordinate. The polar stratospheric downward mass flux in winter is found to be much larger in the NH than in the SH.
format Report
author イワサキ トシキ
Toshiki IWASAKI
spellingShingle イワサキ トシキ
Toshiki IWASAKI
MEAN-MERIDIONAL CIRCULATION OF THE POLAR STRATOSPHERE REPRODUCED IN A GCM
author_facet イワサキ トシキ
Toshiki IWASAKI
author_sort イワサキ トシキ
title MEAN-MERIDIONAL CIRCULATION OF THE POLAR STRATOSPHERE REPRODUCED IN A GCM
title_short MEAN-MERIDIONAL CIRCULATION OF THE POLAR STRATOSPHERE REPRODUCED IN A GCM
title_full MEAN-MERIDIONAL CIRCULATION OF THE POLAR STRATOSPHERE REPRODUCED IN A GCM
title_fullStr MEAN-MERIDIONAL CIRCULATION OF THE POLAR STRATOSPHERE REPRODUCED IN A GCM
title_full_unstemmed MEAN-MERIDIONAL CIRCULATION OF THE POLAR STRATOSPHERE REPRODUCED IN A GCM
title_sort mean-meridional circulation of the polar stratosphere reproduced in a gcm
publisher Japan Meteorological Agency
publishDate 1992
url https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=3695
http://id.nii.ac.jp/1291/00003695/
https://nipr.repo.nii.ac.jp/?action=repository_action_common_download&item_id=3695&item_no=1&attribute_id=18&file_no=1
genre Polar meteorology and glaciology
Proceedings of the NIPR Symposium on Polar Meteorology and Glaciology
genre_facet 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=3695
http://id.nii.ac.jp/1291/00003695/
AA10756213
Proceedings of the NIPR Symposium on Polar Meteorology and Glaciology, 5, 24-28(1992-02)
https://nipr.repo.nii.ac.jp/?action=repository_action_common_download&item_id=3695&item_no=1&attribute_id=18&file_no=1
_version_ 1766171959025991680

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