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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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樓主: FERN
41#
發(fā)表于 2025-3-28 17:56:10 | 只看該作者
42#
發(fā)表于 2025-3-28 22:41:53 | 只看該作者
43#
發(fā)表于 2025-3-29 02:04:30 | 只看該作者
44#
發(fā)表于 2025-3-29 06:41:22 | 只看該作者
45#
發(fā)表于 2025-3-29 10:54:53 | 只看該作者
https://doi.org/10.1007/978-94-011-5058-3Absorption; Cloud; Ocean; Scale; Weather forecasting; Wind; convection
46#
發(fā)表于 2025-3-29 12:22:01 | 只看該作者
978-94-010-6125-4Springer Science+Business Media Dordrecht 1998
47#
發(fā)表于 2025-3-29 17:39:37 | 只看該作者
48#
發(fā)表于 2025-3-29 19:48:18 | 只看該作者
Matrices with Real or Complex Entries,te “The scientific study of turbulent flow spans approximately one hundred years; during that time some of the greatest names in physics, mechanics, and engineering have at one time or another taken a crack at the problem. Progress in many directions has been made, indeed significant progress. However, the ‘turbulence problem’ …remains. ”
49#
發(fā)表于 2025-3-30 00:40:38 | 只看該作者
50#
發(fā)表于 2025-3-30 04:52:53 | 只看該作者
Matrices with Real or Complex Entries,e rate of convective transport defines a buoyancy velocity, which is used to parameterize surface heat, moisture, and momentum fluxes (drag). Vertical profiles of wind and potential temperature are found for the radix layer, the bottom fifth of the boundary layer, which work better than classical surface-layer similarity theories.
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