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Titlebook: Environmental Stratified Flows; Vincenzo Armenio,Sutanu Sarkar Book 2005 CISM Udine 2005 Layer.fluid mechanics.geophysical fluid dynamic.m

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发表于 2025-3-21 17:23:45 | 显示全部楼层 |阅读模式
书目名称Environmental Stratified Flows
编辑Vincenzo Armenio,Sutanu Sarkar
视频video
丛书名称CISM International Centre for Mechanical Sciences
图书封面Titlebook: Environmental Stratified Flows;  Vincenzo Armenio,Sutanu Sarkar Book 2005 CISM Udine 2005 Layer.fluid mechanics.geophysical fluid dynamic.m
描述Stratified flows, common in environmental and geophysical applications, are char­ acterized by the variation of fluid density in the vertical direction that can result in qualitative and quantitative modifications of the flow patterns by buoyancy . Unstable stratification (dense water/air above light water/air) increases the ver­ tical mixing by generation of convective cells while stable stratification generally suppresses vertical mixing of mass and momentum. Even so, a stably stratified fluid can support internal waves, instabilities and turbulence that play a critical role in transport and mixing. The ocean is predominantly subject to stable stratification which, under exter­ nal excitation, supports an environment of internal waves which may then break and generate turbulence. Wind forcing, currents and convective plumes are other sources of turbulence in the ocean. In the ocean, stratified turbulence mediates the upward transport of bottom water, nutrients, chemical and biological species, and pollutants. In the atmosphere, stratification affects the transport of pollutants released at ground level, a critical problem being the thermal inversion in urban areas that causes the
出版日期Book 2005
关键词Layer; fluid mechanics; geophysical fluid dynamic; mathematical modeling; mechanics; mixing; modeling; turb
版次1
doihttps://doi.org/10.1007/3-211-38078-7
isbn_softcover978-3-211-28408-7
isbn_ebook978-3-211-38078-9Series ISSN 0254-1971 Series E-ISSN 2309-3706
issn_series 0254-1971
copyrightCISM Udine 2005
The information of publication is updating

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发表于 2025-3-21 22:47:52 | 显示全部楼层
Internal gravity waves in geophysical fluids,lustrate the occurence of stably-stratified flows in nature and, in Section 2, we derive the Boussinesq approximation. Except for a very brief presentation of the Kelvin-Helmholtz instability in Section 3, we start discussing about internal gravity waves from this section on. The linear properties o
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Internal gravity waves in geophysical fluids,yancy-induced instabilities (Section 4), interaction with a shear flow (Section 5), interaction with a sloping boundary (Section 6). We briefly discuss about the statistical properties of the breaking wave field in Section 7 and introduce some notions on mixing in Section 8.
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Contributions to Political Science 2 also deals with Large-eddy simulation of stratified turbulent flows. Models widely in use for the closure of the subgrid scale stresses are described and recent achievements in the field of stratified flows discussed. Section 3 is devoted to the description of very recent numerical results for stratified flows over a topography.
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Mathematical modeling of Stratified flows, 2 also deals with Large-eddy simulation of stratified turbulent flows. Models widely in use for the closure of the subgrid scale stresses are described and recent achievements in the field of stratified flows discussed. Section 3 is devoted to the description of very recent numerical results for stratified flows over a topography.
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