Titlebook: Nonlinear Processes in Geophysical Fluid Dynamics; A tribute to the sci O. U. Velasco Fuentes,J. Sheinbaum,J. Ochoa Book 2003 Springer Scie

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Overview: 978-94-010-3996-3978-94-010-0074-1

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Deep Ocean Influence on Upper Ocean Baroclinic Instability Saturation,egion. We also found that the size of state space available for eddy-amplitude growth tends to minimize in this same region. Moreover, we found that for a large spread of parameter values in this region the latter size reduces to only a small fraction of the total enstrophy of the system, thereby al

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,Baroclinic Waves in Climates of the Earth’s Past, factors-the distribution of incoming solar radiation, atmospheric greenhouse gases, and topograhic forcing-affect the mean baroclinic structure of our atmosphere, the amount of baroclinic wave activity present, and the eddy heat and momentum fluxes associated with these eddies. The equatorward flux

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Residual Flow and Mixing in the Large Islands Region of the Central Gulf of California,ir spatial variability on the total current field. Strong mixing is caused by the tidal flow, both by friction against the bottom and in the interior of the fluid. Mixing is tidally modulated, at the diurnal, semidiurnal and fortnightly frequencies. The strongest mixing occurs over and close to the