Titlebook: Ocean Modeling and Parameterization; Eric P. Chassignet,Jacques Verron Book 1998 Springer Science+Business Media Dordrecht 1998 Ocean.Pote

irradicable

Antagonist

STRIA

暂时别动

考博

Parameterization of the Fair Weather Ekman Layer,diurnal cycle is likely to be important in fair weather conditions. The process of diurnal cycling can be treated in a layered model to yield a closed solution for Ekman layer currents. This solution has some of the characteristics of a useful parameterization for use in an OGCM, though it covers only a part of the relevant parameter range.

旧石器

Marginal Sea Overflows for Climate Simulations,Compared to an OGCM solution without a marginal sea, but one which still has a vigorous thermohaline circulation, the combined model solution has much better deep water properties and a rather different circulation in the northern basin.

可以任性

Interleaving at the Equator,ameters used in subgrid scale processes. McPhaden [.] notes the importance of improving model physics, through parameterizing small scale mixing processes, to accurately model the equatorial ocean and predict El Niño.

公式

Statistical Mechanics of Potential Vorticity for Parameterizing Mesoscale Eddies,e drift term corresponds to the Neptune effect of Holloway (.). Application to a wind-driven barotropic ocean basin is presented, and extensions to baroclinic cases are sketched. A more mechanistic approach, using kinetic models, confirms the existence of the drift term and estimates the diffusivity.

蹒跚

Book 1998 representation of the differential equations by their algebraic analogs. Equally significant, if not more so, has been the improved under­ standing of physical processes on space and time scales smaller than those that can be represented in such models. Today, some of the most challeng­ ing issues

滋养

Modeling and Parameterizing the Ocean Planetary Boundary Layer,e OBL. The ocean’s benthic boundary layer and its parameterization are the subjects of Beckmann (1998, this volume). Shallow coastal regions where the OBL and benthic boundary layer interact, and where ocean tidal mixing can be strong are excluded. Also excluded are ocean interior mixing processes, except when they interact with the OBL.