Baroclinic instability of an idealized model of the polar night jet
Abstract The zonal current u ( z ), considered by Murray (1960, Section 4), as a model for the polar night jet in the lower stratosphere, has no shear in the model troposphere, and constant vertical shear u z in the stratosphere, u being a continuous function of z . The Richardson number is large. I...
| Published in: | Quarterly Journal of the Royal Meteorological Society |
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| Main Author: | |
| Format: | Article in Journal/Newspaper |
| Language: | English |
| Published: |
Wiley
1972
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| Online Access: | http://dx.doi.org/10.1002/qj.49709841513 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fqj.49709841513 https://rmets.onlinelibrary.wiley.com/doi/pdf/10.1002/qj.49709841513 |
| Summary: | Abstract The zonal current u ( z ), considered by Murray (1960, Section 4), as a model for the polar night jet in the lower stratosphere, has no shear in the model troposphere, and constant vertical shear u z in the stratosphere, u being a continuous function of z . The Richardson number is large. It is shown that this zonal current is always unstable, in the absence of dissipation, to small‐amplitude wave disturbances of essentially the same kind as those found in the theories of Charney and Eady. But, for numerical parameter values appropriate to the base of the polar night jet, predicted growth rates are small, and the disturbances have high zonal wave number (say 5 to 10) and are not very deep (several km at most). |
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