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

领袖气质

Interleaving at the Equator,ent studies have shown that for the ENSO phenomenom the predictability of coupled models is very dependent on the initial state of the ocean model (. Latif and Graham, [.]). What dictates the state of the ocean, its density and current structure, is still a matter for debate. Neelin . [.] suggest th

generic

Eddy Parameterisation in Large Scale Flow,en the need for simulations of centuries to examine climate issues, and the enormous computer resources necessary to undertake such integrations while retaining at least some degree of eddy activity in the model. For the foreseeable future, climate models will have to continue to include parameteris

教唆

誓言

Statistical Mechanics of Potential Vorticity for Parameterizing Mesoscale Eddies,ded diffusion current) in parameterizing the diffusion of a conserved quantity. In the case of potential vorticity, complete mixing is forbidden by energy conservation, and the MEP leads to a subgrid-scale parameterization with a diffusion term, but also with a drift term. The end result of the free

Priapism

Topographic Stress: Importance and Parameterization,ced by the break up of the continents. This nonlinear nature of ocean dynamics generates a wide variety of interesting physical phenomena mainly related to the existence of strong dynamical links among physical processes occurring at different space and time scales. These links range from space scal

不能平静

CRAMP

粉笔

,On the Large-Scale Modeling of Sea Ice and Sea Ice—Ocean Interactions,nd slow current rivers, sea ice forms not only at the surface but also underwater. This is due to the fact that, for typical ocean salinities, the seawater density increases monotonically with decreasing temperature, and therefore surface cooling generates continued convective overturning until the

拱形大桥

Antagonist

Forcing the Ocean,onto the abyssal plain. The entire budget for the world ocean is roughly 10.., which is thought to be carried by the hydrothermal part; the conductive part is a similar order of magnitude. For comparison, the annual mean solar heat flux entering the ocean from the sea surface is above 150 .. on aver