OGLE 发表于 2025-3-23 10:59:33
Modeling the Oceanic Mixed-Layer and Effects of Deep Convection,opriate information on the fluxes at the air-sea interface. Most coupled models with simplified fluxes do not represent the surface temperature well enough and water mass characteristics drift away from the initial state. Restoring conditions at the sea surface are needed to force the model back toIntruder 发表于 2025-3-23 14:37:24
Observations of Clear and Cloud-Capped Convective Boundary Layers, and Techniques for Probing Them,lecting and absorbing solar radiation (globally they reflect about 20% of the total incoming radiation), and, if deep enough, by generating their own secondary circulations through the release of latent heat by condensation. In this way, clouds are a mechanism for releasing latent heat emitted from亚当心理阴影 发表于 2025-3-23 22:02:37
Bulk Models of the Atmospheric Convective Boundary Layer,umptions of the zero-order representation of the CBL vertical structure. The developed theory is generalized for the case of the CBL over an irregular terrain..The second model considered is the general-structure CBL bulk model, which incorporates a self-similar representation of the buoyancy profil浪费物质 发表于 2025-3-24 01:33:05
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Book 1998 andmicrophysics. New theoretical concepts and approaches have beenoutlined regarding scaling and parameterization of physical processesin buoyancy-driven geophysical flows. .The book summarizes interdisciplinary studies of buoyancy effects indifferent media (atmosphere and hydrosphere) over a wideDelude 发表于 2025-3-24 10:55:09
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Experiment, Numerical Modeling, Numerical Simulation, and Their Roles in the Study of Convection,A casual observer of a turbulent flow, say a cigarette plume or the eddying motion downstream of a waterfall, can easily get the impression that turbulence behaves as it pleases locally in space and time. Any constraints on its behavior seem to come with a long leash.集合 发表于 2025-3-24 21:39:03
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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. Howev