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...
Main Authors: | , , , |
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Format: | Text |
Language: | English |
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Online Access: | http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.608.4155 http://www.cpom.org/research/jcrh-procissf.pdf |