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Diagnosing Ocean Unstable Baroclinic Waves and Meanders Using the Quasigeostrophic Equations and Q-Vector Method
baroclinic waves wave growth rate
2008/11/18
A three-dimensional, primitive equation model is applied to the ocean mesoscale eddies and unstable baroclinic waves across a density front in a channel under a very low viscosity environment. Current...
Japan Sea Thermohaline Structure and Circulation. Part II: A Variational P-Vector Method
Japan Sea Thermohaline Structure Circulation P-Vector Method
2008/7/31
The second part of this work investigates the seasonal variabilities of the Japan/East Sea (JES) circulation using the U.S. Navy Generalized Digital Environmental Model (GDEM) climatological temperatu...