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Titlebook: Ocean Processes in Climate Dynamics; Global and Mediterra Paola Malanotte-Rizzoli,Allan R. Robinson Book 1994 Springer Science+Business Med

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發(fā)表于 2025-3-25 06:41:32 | 只看該作者
22#
發(fā)表于 2025-3-25 11:17:06 | 只看該作者
Sensitivity Studies on the Role of the Ocean in Climate Change,Ocean circulation. These experiments make use of the GFDL primitive equation model with 30 vertical levels and 1.0° × 1.2° horizontal resolution. The nature of the heat flux forcing and the importance of the implied evaporation minus precipitation (salinity) forcing will be described and the consequ
23#
發(fā)表于 2025-3-25 14:07:41 | 只看該作者
Modeling the Wind and Thermohaline Circulation in the North Atlantic Ocean, Center for Atmospheric Research in Boulder and at the Institut für Meereskunde in Kiel. In this series, a variety of experiments has been performed using the GFDL primitive equation model at 1/3° × 2/5° latitude-longitude resolution, examining sensitivity to surface forcing and parameterization cho
24#
發(fā)表于 2025-3-25 18:35:39 | 只看該作者
Studying Thermohaline Circulation in the Ocean by Means of Transient Tracer Data,w investigation of thermohaline circulation of the ocean and of interior-ocean mixing. Features of the tracers and their distributions are outlined, and examples are given of oceanographic studies employing tracer data. Spreading of surface waters into the interior ocean and pathways of certain deep
25#
發(fā)表于 2025-3-25 20:55:05 | 只看該作者
26#
發(fā)表于 2025-3-26 01:48:20 | 只看該作者
Open Ocean Deep Convection, Mediterranean and Greenland Seas,w 100 m horizontal scale during cooling periods, in agreement with scaling arguments and non-hydrostatic modelling results. The integral effect of the plumes is that of a mixing agent rather than carrying water downward in a mean motion. It depends on the intensity and duration of the cooling how co
27#
發(fā)表于 2025-3-26 06:46:44 | 只看該作者
28#
發(fā)表于 2025-3-26 11:27:36 | 只看該作者
29#
發(fā)表于 2025-3-26 15:58:03 | 只看該作者
30#
發(fā)表于 2025-3-26 19:17:26 | 只看該作者
Modeling the General Circulation of the Mediterranean,ed questions related to it. Then, ongoing modeling efforts are presented that focus upon different aspects of the circulation, such as the wind-driven and/or the thermohaline components; the seasonal versus the yearly variability; the importance of the inflow at the straits, the Strait of Gibraltar
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