MEAN-MERIDIONAL CIRCULATION OF THE POLAR STRATOSPHERE REPRODUCED IN A GCM
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概要
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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.
- 国立極地研究所の論文