Article ID | Journal | Published Year | Pages | File Type |
---|---|---|---|---|
4552736 | Ocean Modelling | 2007 | 16 Pages |
Abstract
The overshootings and oscillations are induced by the strong damping of the smaller scale modes and are therefore comparable to the Gibbs' phenomenon. With appropriate boundary conditions, the variance of the field decreases monotonically and the oscillations are expected to remain small. The lack of positiveness is however a severe drawback for (dynamic) tracer studies.
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Atmospheric Science
Authors
Ãric J.M. Delhez, Ãric Deleersnijder,