| 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.
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													Atmospheric Science
												
											Authors
												Ãric J.M. Delhez, Ãric Deleersnijder, 
											