Ondines-curse
发表于 2025-3-23 10:37:28
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
发表于 2025-3-23 15:31:07
,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
发表于 2025-3-23 19:26:57
http://reply.papertrans.cn/23/2277/227690/227690_13.png
北极人
发表于 2025-3-24 00:54:30
http://reply.papertrans.cn/23/2277/227690/227690_14.png
人造
发表于 2025-3-24 04:24:49
http://reply.papertrans.cn/23/2277/227690/227690_15.png
哥哥喷涌而出
发表于 2025-3-24 07:33:53
http://reply.papertrans.cn/23/2277/227690/227690_16.png
准则
发表于 2025-3-24 13:41:27
http://reply.papertrans.cn/23/2277/227690/227690_17.png
军械库
发表于 2025-3-24 16:47:20
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
发表于 2025-3-24 19:30:32
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
发表于 2025-3-25 02:36:49
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