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Titlebook: Ocean Modeling and Parameterization; Eric P. Chassignet,Jacques Verron Book 1998 Springer Science+Business Media Dordrecht 1998 Ocean.Pote

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發(fā)表于 2025-3-21 19:11:01 | 只看該作者 |倒序?yàn)g覽 |閱讀模式
書目名稱Ocean Modeling and Parameterization
編輯Eric P. Chassignet,Jacques Verron
視頻videohttp://file.papertrans.cn/701/700497/700497.mp4
叢書名稱Nato Science Series C:
圖書封面Titlebook: Ocean Modeling and Parameterization;  Eric P. Chassignet,Jacques Verron Book 1998 Springer Science+Business Media Dordrecht 1998 Ocean.Pote
描述The realism of large scale numerical ocean models has improved dra- matically in recent years, in part because modern computers permit a more faithful representation of the differential equations by their algebraic analogs. Equally significant, if not more so, has been the improved under- standing of physical processes on space and time scales smaller than those that can be represented in such models. Today, some of the most challeng- ing issues remaining in ocean modeling are associated with parameterizing the effects of these high-frequency, small-space scale processes. Accurate parameterizations are especially needed in long term integrations of coarse resolution ocean models that are designed to understand the ocean vari- ability within the climate system on seasonal to decadal time scales. Traditionally, parameterizations of subgrid-scale, high-frequency mo- tions in ocean modeling have been based on simple formulations, such as the Reynolds decomposition with constant diffusivity values. Until recently, modelers were concerned with first order issues such as a correct represen- tation of the basic features of the ocean circulation. As the numerical simu- lations become better
出版日期Book 1998
關(guān)鍵詞Ocean; Potential; Sea ice; computer; convection; dynamics; mixing; turbulent flow
版次1
doihttps://doi.org/10.1007/978-94-011-5096-5
isbn_softcover978-0-7923-5229-7
isbn_ebook978-94-011-5096-5Series ISSN 1389-2185
issn_series 1389-2185
copyrightSpringer Science+Business Media Dordrecht 1998
The information of publication is updating

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Forcing the Ocean,ins…”, and it could continue as: “… and therefore the physical boundaries of the ocean are the bottom of the basins, the coastlines, and the free surface in permanent contact with the atmosphere”. Heat entering the ocean through the bottom of the basins is usually considered as negligible. Estimates
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Parameterization of the Fair Weather Ekman Layer,re and compared with fair weather data sets. A steady classical diffusion model is found to give reasonably good simulations with familiar values of diffusivity. However, the solutions show a systematic error in current direction that arises, apparently, from a non-parallel relation between shear an
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Turbulent Mixing in the Ocean,of order 10.m) are limited chiefly by the size of ocean basins and ultimately of the earth. On the other end of the spectrum, gradients in velocity and water properties exist to sub-meter scales (see below). The total range of spatial scales is thus some nine or more orders of magnitude. The tempera
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Double-Diffusive Convection, of the two orders of magnitude difference between the thermal conductivity of water and the diffusivity of dissolved salts, and the tendency of gradients of temperature and salinity to oppose one another in their effects on density. This leads to a number of counter-intuitive effects, such as up-gr
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