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Titlebook: IUTAM Symposium on Advances in Mathematical Modelling of Atmosphere and Ocean Dynamics; Proceedings of the I P. F. Hodnett Conference proce

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發(fā)表于 2025-3-21 16:10:36 | 只看該作者 |倒序?yàn)g覽 |閱讀模式
書(shū)目名稱IUTAM Symposium on Advances in Mathematical Modelling of Atmosphere and Ocean Dynamics
副標(biāo)題Proceedings of the I
編輯P. F. Hodnett
視頻videohttp://file.papertrans.cn/461/460550/460550.mp4
叢書(shū)名稱Fluid Mechanics and Its Applications
圖書(shū)封面Titlebook: IUTAM Symposium on Advances in Mathematical Modelling of Atmosphere and Ocean Dynamics; Proceedings of the I P. F. Hodnett Conference proce
描述The goals ofthe Symposium were to highlight advances in modelling ofatmosphere and ocean dynamics, to provide a forum where atmosphere and ocean scientists could present their latest research results and learn ofprogress and promising ideas in these allied disciplines; to facilitate interaction between theory and applications in atmosphere/ocean dynamics. These goals were seen to be especially important in view ofcurrent efforts to model climate requiring models which include interaction between atmosphere, ocean and land influences. Participants were delighted with the diversity ofthe scientific programme; the opportunity to meet fellow scientists from the other discipline (either atmosphere or ocean) with whom they do not normally interact through their own discipline; the opportunity to meet scientists from many countries other than their own; the opportunity to hear significant presentations (50 minutes) from the keynote speakers on a range ofrelevant topics. Certainly the goal ofcreating a forum for exchange between atmosphere and ocean scientists who need to input to create realistic models for climate prediction was achieved by the Symposium and this goal will hopefully be f
出版日期Conference proceedings 2001
關(guān)鍵詞Coast; Inversion; Ocean; Scale; Storm; Weather forecasting; marine
版次1
doihttps://doi.org/10.1007/978-94-010-0792-4
isbn_softcover978-94-010-3853-9
isbn_ebook978-94-010-0792-4Series ISSN 0926-5112 Series E-ISSN 2215-0056
issn_series 0926-5112
copyrightSpringer Science+Business Media Dordrecht 2001
The information of publication is updating

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Baroclinic Structure of a Modified Stommel-Arons Model of the Abyssal Ocean Circulationen in Levitus (1982) when the vertical coefficient of thermal diffusion is 125 × 10...s.. The vertical, meridional and zonal components of velocity show significant change in structure from the Stommel — Arons expressions.
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Open Boundary Conditions: Fact and Fiction to avoid possible problems at the lateral boundaries of a limited domain. Moreover, in a fluid such as the atmosphere there is no distinct upper boundary, and most numerical representations of the atmosphere’s vertical structure terminate at some arbitrary level.
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Boundary Filter Initialization of the Hirlam Modelvailable. Such filters have obvious relevance to the problem of initialization for Numerical Weather Prediction. We also discuss some fundamental difficulties encountered when filtering time-limited functions.
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A Dynamical Stabilizer in the Climate System: A Mechanism Suggested by a Simple Model and Supported re known to exist which could, in principle, drive the climate system far from its observed mean state even in the absence of any external forcings. Extreme scenarios that have been envisaged are a completely ice-covered earth on the one hand and a runaway greenhouse such as appears to have occurred on Venus on the other.
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Asymptotic Models and Application to Vortex Dynamicsicyclones travel westward faster than cyclones. In FG, vortices of both signs show initially a secondary meridional northward drift which we detail. However this last feature is not present in RSW numerical simulations. Vortices behave like quasi-geostrophic (QG) vortices i.e, showing an initial meridional drift that depends on vortex sign.
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An Air-Ocean Coupled Nowcast/Forecast System for the East Asian Marginal Sease Gulf of Tonkin to the YES; a deep, elliptical shaped SCS and JES basins, and numerous reef islands and underwater plateaus scattered throughout (Fig. 1a). The shelf that extends from the Gulf of Tonkin to the YES is consistently near 70 m deep, and averages 150 km in width.
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