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

OGLE

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 to

Intruder

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

亞當(dāng)心理陰影

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

浪費(fèi)物質(zhì)

美學(xué)

金哥占卜者

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 wide

Delude

憂傷

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

Arbitrary

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