Titlebook: Climate-Ocean Interaction; M. E. Schlesinger Book 1990 Kluwer Academic Publishers 1990 Ocean.Scale.Sea ice.satellite.temperature

本能

Extratropical Response to SST Anomalies and the Barotropic ModelRecent GCM integrations with El Niño sea surface temperature anomalies are reviewed, and the question of whether the extratropical response can be explained in terms of simple barotropic model dynamics is examined.

盘旋

General Circulation Modelling of the Atmospheres of the Meteorological Office AGCM are presented and assessed against climatological data. Examples are given of the changes in surface fluxes in numerical experiments with CO.. Finally, the problems of coupling atmosphere and ocean models are discussed and future advances in atmospheric modelling are considered.

Kindle

Little

Modelling of Geochemical Tracers in the Oceanonal current field of an OGCM. The modelled tracers are phosphate, alkalinity, oxygen, dissolved inorganic carbon, particulate organic carbon, and calcite, the latter three in three isotopes. By an appropriate choice of inventories and metabolic rates, a satisfactory agreement with data, especially the GEOSECS data, could be achieved.

GORGE

Silent-Ischemia

神经

,Das natürliche elektromagnetische Umfeld,ations contributing to these are presented where relevant. Preliminary results from a coupled atmosphere/ocean/sea-ice model are discussed in terms of the differences between the transports in the ocean model and those observed.

Agnosia

收养

Rolf Arnold,Marcel Berg,Horst Müller-Petersuse of forcing datasets derived from observed climatology and from an atmospheric general circulation model are described, together with the sensitivity of the sea surface temperature simulation in a coupled atmosphere-ocean model to inclusion of a simple representation of subgrid-scale motions associated with regions of deep convection.

Flounder