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Titlebook: Buoyant Convection in Geophysical Flows; E. J. Plate,E. E. Fedorovich,J. C. Wyngaard Book 1998 Springer Science+Business Media Dordrecht 1

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31#
發(fā)表于 2025-3-26 22:28:12 | 只看該作者
32#
發(fā)表于 2025-3-27 04:18:55 | 只看該作者
Powers of Nonnegative Matrices,thermally stratified wind tunnel of the Institute of Hydrology and Water Resources Planning (IHW), University of Karlsruhe. Design of the wind tunnel, and the technique employed for velocity and temperature measurements are described. The performed experiments reproduce convective conditions in the
33#
發(fā)表于 2025-3-27 05:36:55 | 只看該作者
Powers of Nonnegative Matrices, and stable boundary layer. For a review of the meteorological characteristics of the three prototypes we refer to Nieuwstadt and Duynkerke [10]. Here we shall concentrate on the CBL. Convection or rather the term free convection is used to describe the process whereby turbulence is produced by buoy
34#
發(fā)表于 2025-3-27 11:32:54 | 只看該作者
35#
發(fā)表于 2025-3-27 16:04:25 | 只看該作者
Matrices in Engineering Problemsn the large-scale subsiding motion is strong and the ocean surface is cold. This large-scale condition leads to a very moist, shallow planetary boundary layer (PBL). The lifting condensation level is below the top of the mixed layer, so an uniform layer of cloud can form in the upper part of the PBL
36#
發(fā)表于 2025-3-27 18:06:31 | 只看該作者
37#
發(fā)表于 2025-3-28 00:15:38 | 只看該作者
Nato Science Series C:http://image.papertrans.cn/b/image/191960.jpg
38#
發(fā)表于 2025-3-28 03:21:04 | 只看該作者
39#
發(fā)表于 2025-3-28 06:16:25 | 只看該作者
Eddy Dynamics and Kinematics of Convective Turbulence, these are related to the interactions of the turbulence with the rigid surfaces and other regions of fluid motion bounding the convective layer. The effects of weak cross winds and non-uniformity in surface conditions are also discussed.
40#
發(fā)表于 2025-3-28 11:21:34 | 只看該作者
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