LURE
发表于 2025-3-25 06:38:26
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描述
发表于 2025-3-25 10:48:18
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下边深陷
发表于 2025-3-25 13:09:23
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, Bäuerle, 1986) will be investigated. Finally section 5.6 presents solutions in curved channels.
IRS
发表于 2025-3-25 18:40:09
978-3-540-17623-7Springer-Verlag Berlin Heidelberg 1987
vasospasm
发表于 2025-3-25 22:19:26
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synovitis
发表于 2025-3-26 02:48:57
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.
HARP
发表于 2025-3-26 07:54:53
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.
珍奇
发表于 2025-3-26 12:10:37
Coastal and Estuarine Studieshttp://image.papertrans.cn/u/image/926346.jpg
Dorsal-Kyphosis
发表于 2025-3-26 12:58:01
https://doi.org/10.1007/978-3-642-50990-2Oscillation; dispersion; lake; numerical method; ocean; wave; wave equation
chronology
发表于 2025-3-26 17:27:17
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