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

Ondines-curse

Climatic Change and Ocean Bottom Water Formation: Are We Missing Something?pwelling over all the world’s oceans. Relatively shallow, thermally-driven convective overturning occurring at high latitudes which arises from heating of the atmosphere by the oceans is fairly well represented in current numerical ocean models, but deep convection from surface salinity sources incl

seroma

,Das natürliche elektromagnetische Umfeld,ttention is primarily given to the annual-mean fields which are of significance for long-term trends in climate, although aspects of the seasonal variations contributing to these are presented where relevant. Preliminary results from a coupled atmosphere/ocean/sea-ice model are discussed in terms of

Leaven

北極人

人造

哥哥噴涌而出

準則

軍械庫

Sicherheitsversprechen im Wandeln Oscillation (ENSO) phenomenon are briefly reviewed. The studies described encompass the investigation of the atmospheric response to observed sea surface temperatures (SSTs), the oceanic response to observed wind stresses, and studies with coupled ocean-atmosphere models investigating large-scale

冰河期

Rolf Arnold,Marcel Berg,Horst Müller-Petersds of providing the non-interactive forcing for ocean circulation models are reviewed and the sensitivities of a model of the tropical Pacific to the use of forcing datasets derived from observed climatology and from an atmospheric general circulation model are described, together with the sensitivi

新手

Risikokompetenz und deren Hemmnisseonal 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