Article ID Journal Published Year Pages File Type
4552736 Ocean Modelling 2007 16 Pages PDF
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
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