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
Description
Summary: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.

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