Titlebook: Oceanic Circulation Models: Combining Data and Dynamics; David L. T. Anderson,Jürgen Willebrand Book 1989 Kluwer Academic Publishers 1989

TUMOR

書目名稱Oceanic Circulation Models: Combining Data and Dynamics影響因子(影響力)




書目名稱Oceanic Circulation Models: Combining Data and Dynamics影響因子(影響力)學科排名




書目名稱Oceanic Circulation Models: Combining Data and Dynamics網絡公開度




書目名稱Oceanic Circulation Models: Combining Data and Dynamics網絡公開度學科排名




書目名稱Oceanic Circulation Models: Combining Data and Dynamics被引頻次




書目名稱Oceanic Circulation Models: Combining Data and Dynamics被引頻次學科排名




書目名稱Oceanic Circulation Models: Combining Data and Dynamics年度引用




書目名稱Oceanic Circulation Models: Combining Data and Dynamics年度引用學科排名




書目名稱Oceanic Circulation Models: Combining Data and Dynamics讀者反饋




書目名稱Oceanic Circulation Models: Combining Data and Dynamics讀者反饋學科排名

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Synchronism

2否定

Determining Diffusivities from Hydrographic Data by Inverse Methods with Applications to the Circum has been generalized in this respect (see e.g. Wunsch 1984). We should also mention Hogg’s model (Hogg 1987) which is an inversion of the advective-diffusive balances on two isopycnals subject to the geostrophic constraint between the isopycnals. The model was applied in the central North Atlantic.

松軟無力

,Altimeter Data Assimilation into Ocean Circulation Models — Some Preliminary Results,ole in that they must be able to successfully extrapolate surface observational information downward into the ocean interior if they are to achieve success in reconstructing a realistic ocean circulation.

Diastole

Book 1989ith using models to infer the ocean circulation. Understanding our climate is one of the major problems of the late twentieth century. The possible climatic changes resulting from the rise in atmospheric carbon dioxide and other trace gases are of primary interest and the ocean pla. ys a ma. jor rol

compassion

1389-2185 oncerned with using models to infer the ocean circulation. Understanding our climate is one of the major problems of the late twentieth century. The possible climatic changes resulting from the rise in atmospheric carbon dioxide and other trace gases are of primary interest and the ocean pla. ys a m

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Introduction to Chemical Tracers of the Ocean Circulation,at play at the air-sea interface and how they affect the tracer concentrations at the surface. Finally in section 4 two recent studies on how tracers constrain diapycnal mixing in the deep ocean are discussed.

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Assimilation of XBT Data Using a Variational Technique,ns from this preliminary field. Operationally, a short range forecast constitutes the preliminary field. Constraints on the time evolution of the system are not imposed, since O.I. (as currently used) is an analysis at a single time.

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