Large-scale baroclinic and barotropic instabilities, Eady and Charney models for baroclinic instability, and energy transfer. Response of the ocean to transient and steady winds and buoyancy forcing.

Stammer, D. Ray, R. D. Andersen, O. B. Arbic, B. K. Bosch, W. Carrère, L. Cheng, Y. Chinn, D. S. Dushaw, B. D. Egbert, G. D. Erofeeva, S. Y. Fok, H. S. Green, J. A ...

The remnants of Hurricane Francine and a barotropic (vertically aligned in the atmosphere) system remain stationary over the east coast of the Carolinas, creating a strong blocking pattern across the ...

Abstract: We investigate the cross-equatorial flow of deep ocean currents through a channel along the sea floor using the 1½-layer or equivalent-barotropic shallow water equations. We restrict our ...

barotropic ocean model. We show the improvement in terms of reduction of variance of 15 different superconducting gravimeters of the worldwide Global Geodynamics Project (GGP) network, compared to the ...

Katherine J. Evans directs the Office of Institutional Strategic Planning at Oak Ridge National Laboratory. Prior to her current role, she served as director of ORNL's Computational Sciences and ...

A simple but very practical Eulerian forward-backward method was adopted to replace the most preferred leapfrog scheme as the time-differencing method for both barotropic and baroclinic modes. The ...

Chen, Nan and Majda, Andrew J. 2017. Beating the curse of dimension with accurate statistics for the Fokker–Planck equation in complex turbulent systems. Proceedings of the National Academy of ...

Coexistence of ecologically similar species occupying the same geographic location (sympatry) poses questions regarding how their populations persist without leading to competitive exclusion. There is ...

The Rossby wave source is a term used to describe the mechanisms that generate and maintain Rossby waves. The RWS was derived from the barotropic vorticity equation in pressure coordinates e.g., ...