Article ID | Journal | Published Year | Pages | File Type |
---|---|---|---|---|
4552317 | Ocean Modelling | 2011 | 7 Pages |
Abstract
⺠Large time steps for efficient calculation of slow modes in an ocean model. ⺠High-order explicit treatment of the slow modes and the long-wave parts of the fast barotropic mode. ⺠Only the short-wave part of the fast barotropic mode is calculated implicitly. ⺠Obviates the need for a fully-converged iterative solution to the elliptic equation for surface elevation.
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Atmospheric Science
Authors
Brian G. Sanderson,