Downward migration of extratropical zonal wind anomalies

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چکیده

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Downward migration of extratropical zonal wind anomalies

We show (in confirmation of previous work) using oneand three-dimensional models that extratropical zonal wind anomalies, produced by fluctuating Rossby wave forcing in the troposphere, appear first in the stratosphere, and migrate downward into the troposphere. By systematically eliminating wave reflection and “downward control” through an induced meridional circulation, it is shown that the d...

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ژورنال

عنوان ژورنال: Journal of Geophysical Research

سال: 2003

ISSN: 0148-0227

DOI: 10.1029/2002jd002773