Instability and nonlinear equilibration of baroclinic flows
Baroclinic instability, the fundamental mechanism underlying the generation of baroclinic eddies in the atmosphere and ocean is investigated in the two-layer, quasi-geostrophic model. The aim is to bridge the gap in understanding between analytical theories and high resolution numerical simulations...
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University College London (University of London)
2012
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| Online Access: | http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.565807 |