標(biāo)題: Titlebook: Topographic Waves in Channels and Lakes on the f-Plane; Thomas Stocker,Kolumban Hutter Textbook 1987 Springer-Verlag Berlin Heidelberg 198 [打印本頁(yè)] 作者: 去是公開(kāi) 時(shí)間: 2025-3-21 17:35
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作者: EWE 時(shí)間: 2025-3-21 23:25
Thomas Stocker,Kolumban Hutterctures and applications‘. It appears somewhat later than is perhaps desirable for a volume resulting from a summer school. In return it contains a good many results which were not yet available at the time of the meeting. In particular it is now abundantly clear that the Deformation theory of algebr作者: landmark 時(shí)間: 2025-3-22 01:49
Thomas Stocker,Kolumban Hutterlic loading under uniaxial tension-compression and standard temperature is used to identify some features and dissimilarities of isotropic and anisotropic hardening processes that occur during monotonic and cyclic loading. In order to describe these features in terms of the plasticity theory (the Bo作者: Abnormal 時(shí)間: 2025-3-22 08:10 作者: arabesque 時(shí)間: 2025-3-22 12:05
Thomas Stocker,Kolumban Huttermaterial science.Describes structure-property relationships .This book describes the properties of single polymer molecules and polymeric materials and the methods how to characterize them. Molar masses, molar mass distributions and branching structure are discussed in detail. These properties are d作者: lobster 時(shí)間: 2025-3-22 14:00 作者: Entirety 時(shí)間: 2025-3-22 20:50
Thomas Stocker,Kolumban Hutterntitative description of the toughness behaviour by means of fracture mechan- ics parameters and enables preventive failure analysis. In recent years this young scientific discipline has developed rapidly, and now the experimental results are looking for more applications in industrial practice. How作者: Nefarious 時(shí)間: 2025-3-23 01:07
Thomas Stocker,Kolumban Hutterm polyethylene single crystals. The observations by transmission electron microscopy and electron diffraction indicate that substrate-free polyethylene crystals fail by brittle fracture at all temperatures between 77 K and 388 K and all strain rates between 10. and 10. sec.. The formation of fibers 作者: 出汗 時(shí)間: 2025-3-23 01:56
following the last deglaciation. As a measure of this variation, sea-level indicators (SLIs) related to the RSL heights at specific past time epochs are used. For the inversion of the RSL-height change in terms of mantle viscosity, neighbouring SLIs may be grouped into an RSL diagram taken as repre作者: 大酒杯 時(shí)間: 2025-3-23 06:23 作者: 小說(shuō) 時(shí)間: 2025-3-23 10:23 作者: needle 時(shí)間: 2025-3-23 13:58
Thomas Stocker,Kolumban Huttern deformation induced anisotropy is considered. The present work addresses the numerical integration of finite deformation plasticity models exhibiting both, isotropic and kinematic hardening. The integration of the evolution equations is based on the elastic predictor and plastic corrector procedur作者: 傀儡 時(shí)間: 2025-3-23 21:36 作者: 不給啤 時(shí)間: 2025-3-24 01:12 作者: 致敬 時(shí)間: 2025-3-24 03:40
ssification scheme of the depositional conditions based on fuzzy logic. After the definition of appropriate membership functions, this method leads to a systematic interpretation of the large number of SLIs available. We apply this method to SLIs from the Richmond-Gulf region, southeastern Hudson Ba作者: nautical 時(shí)間: 2025-3-24 09:54
Topographic waves in rectangular basins,e analytical models to this basin. On the one hand, the elliptical model of Mysak et al. (1985) could explain the 74h-trace in the measurements? it was interpreted as a (1,1)-TW-mode with a . wave pattern.作者: 星球的光亮度 時(shí)間: 2025-3-24 12:16
Textbook 1987raphic Rossby waves in enclosed basins. With this tractate we aim to provide the reader with the basic concepts of wave motion in shallow waters at subinertial frequencies. Our ques- tions throughout this monogra~h are essentially: How can the solutions to this topographic wave equation in a prescri作者: LINES 時(shí)間: 2025-3-24 15:52
Thomas Stocker,Kolumban Huttere applied to the real world there will usually be such things as coefficients which are imperfectly known. Thus it is important to know how the behaviour of a m978-94-010-7875-7978-94-009-3057-5Series ISSN 1389-2185 作者: cartilage 時(shí)間: 2025-3-24 21:38 作者: esthetician 時(shí)間: 2025-3-25 00:49 作者: LURE 時(shí)間: 2025-3-25 06:38 作者: 描述 時(shí)間: 2025-3-25 10:48 作者: 下邊深陷 時(shí)間: 2025-3-25 13:09
Topographic waves in infinite channels,sing the model equations (4.9) and follow Stocker & Hutter (1986a) with additions from Stocker & Hutter (1985). In section 5.5 solutions obtained with analytical and numerical finite difference techniques (Gratton, 1983, Gratton & LeBlond, 1986, B?uerle, 1986) will be investigated. Finally section 5.6 presents solutions in curved channels.作者: IRS 時(shí)間: 2025-3-25 18:40
978-3-540-17623-7Springer-Verlag Berlin Heidelberg 1987作者: vasospasm 時(shí)間: 2025-3-25 22:19 作者: synovitis 時(shí)間: 2025-3-26 02:48
Governing equations,In this chapter we introduce the equations and approximations from which the TW-equation and associated boundary conditions are derived. No completeness is intended.作者: HARP 時(shí)間: 2025-3-26 07:54
Some known solutions of the TW-equation in various domains,Whereas our intentions in chapter 1 have been to suggest that observations of long-periodic oscillations in lakes and ocean basins are likely to be interpretable in terms of vorticity induced motions, we have presented in chapter 2 the basic equations of such waves and analysed the general properties of the associated equations.作者: 珍奇 時(shí)間: 2025-3-26 12:10
Coastal and Estuarine Studieshttp://image.papertrans.cn/u/image/926346.jpg作者: Dorsal-Kyphosis 時(shí)間: 2025-3-26 12:58
https://doi.org/10.1007/978-3-642-50990-2Oscillation; dispersion; lake; numerical method; ocean; wave; wave equation作者: chronology 時(shí)間: 2025-3-26 17:27 作者: MOAN 時(shí)間: 2025-3-26 21:09
Introduction,show pronounced oscillations with a characteristic period of a few days. The existence of such long periodic oscillations in a rotating circular basin with a parabolic depth profile was pointed out by Poincaré in 1910, and the first explicit solution for these topographic waves (also called second c作者: ear-canal 時(shí)間: 2025-3-27 01:16 作者: constitutional 時(shí)間: 2025-3-27 06:02
Topographic waves in infinite channels,sing the model equations (4.9) and follow Stocker & Hutter (1986a) with additions from Stocker & Hutter (1985). In section 5.5 solutions obtained with analytical and numerical finite difference techniques (Gratton, 1983, Gratton & LeBlond, 1986, B?uerle, 1986) will be investigated. Finally section 5作者: 保守黨 時(shí)間: 2025-3-27 12:47
Topographic waves in rectangular basins,ins were found; among these were the conspicuous structure of the lowest modes (linear and quadratic Ball-mode), the counterclockwise phase propagation, the rotation of the velocity vectors, to name a few. In special cases these models allowed satisfactory interpretation of long-periodic phenomena i作者: Deference 時(shí)間: 2025-3-27 16:37 作者: 干涉 時(shí)間: 2025-3-27 18:38
,Review and outlook: Restrictions of this study — A list of unsolved problems,losed basins. As mentioned in the preface, we claim to have achieved a considerable advancement in the understanding of these waves. In particular, it was demonstrated that, besides the free travelling waves, the topographic wave equation admits bound states. These states consist of wave activity wh
