CORIOLIS EFFECTS IN MESOSCALE SHALLOW LAYER FLOWS

A general linearised ‘shallow-layer ’ perturbation model, where the approximately neutral lower layer of thick-ness is situated below a stable upper layer or inversion layer, is developed for idealised and steady, but typical, mesoscale atmospheric flows. Significant Coriolis effects and variations...

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Bibliographic Details
Main Authors: J. C. R. Hunt, A. Orr, D. Cresswell, A. Owinoh
Other Authors: The Pennsylvania State University CiteSeerX Archives
Format: Text
Language:English
Subjects:
Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.605.4502
http://www.cpom.org/research/jcrh-shallow.pdf