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Titlebook: Mesoscale Meteorology - Theories, Observations and Models; Douglas K. Lilly,Tzvi Gal-Chen Book 1983 Springer Science+Business Media B.V. 1

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樓主: DUCT
11#
發(fā)表于 2025-3-23 12:40:06 | 只看該作者
12#
發(fā)表于 2025-3-23 17:01:54 | 只看該作者
Norman A. Crookor IFP, DLP, and ECDLP. It also discusses some quantum resistant cryptosystems to replace the IFP, DLP and ECDLP based cryptosystems..This book is intended to be used either as a graduate text in computing, communications and mathematics, or as a basic reference in the field..978-1-4899-9779-1978-1-4419-7722-9
13#
發(fā)表于 2025-3-23 18:38:23 | 只看該作者
On the Dynamical Definition(s) of “Mesoscale”cing. While these two aspects of fluid behavior lead to energy generation at more or less discrete scales, energy is generally transferred up- and down-scale so that the spectrum of kinetic energy in wavenumber space is smooth, but exhibits peaks..In light of these ideas, we identify several interna
14#
發(fā)表于 2025-3-23 23:13:16 | 只看該作者
Synoptic-Scale Forcing of Mesoscale Processescurred within clearly (if somewhat broadly) defined sectors of synoptic-scale circulations. Although a wide variety of mesoscale phenomena are now recognized, a major share of attention continues to be devoted to precipitation systems, as we shall see. Since virtually all of this wide variety occurs
15#
發(fā)表于 2025-3-24 02:58:20 | 只看該作者
On the Effect of the Planetary Boundary Layer Parameterizations in Mesoscale Numerical Weather Prediferential development of the mixed layer triggered the inland sea breeze effect which led to strong convection and tornado outbreak in the vicinity of Grand Island of Nebraska. The differential surface temperature was caused by downslope adiabatic warming, warm advection, spatial variation in initia
16#
發(fā)表于 2025-3-24 09:23:39 | 只看該作者
Topographic Forcing specific volume and p of pressure from a background state α.(z), T. (z), P. (z) at rest. . stands for frictional forces and F. dc.scribes the influence of subscale motions or radiative cooling on the temperature. Q is a heating rate, f is the Coriolis parameter.
17#
發(fā)表于 2025-3-24 12:33:00 | 只看該作者
18#
發(fā)表于 2025-3-24 17:31:51 | 只看該作者
James E. Hokecomparison results such as for computational simplification by either of two approaches: stochastic monotonicity and ordering results based on the ordering of the process generators, and comparison978-1-4614-2773-5978-1-4419-6472-4Series ISSN 0884-8289 Series E-ISSN 2214-7934
19#
發(fā)表于 2025-3-24 21:02:08 | 只看該作者
Tzvi Gal-Chencomparison results such as for computational simplification by either of two approaches: stochastic monotonicity and ordering results based on the ordering of the process generators, and comparison978-1-4614-2773-5978-1-4419-6472-4Series ISSN 0884-8289 Series E-ISSN 2214-7934
20#
發(fā)表于 2025-3-25 03:11:52 | 只看該作者
Frederick Sanderscomparison results such as for computational simplification by either of two approaches: stochastic monotonicity and ordering results based on the ordering of the process generators, and comparison978-1-4614-2773-5978-1-4419-6472-4Series ISSN 0884-8289 Series E-ISSN 2214-7934
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