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• W2576204857 abstract "A one-dimensional grid-level model including longwave radiative transfer and a level-4 second- order turbulent transfer closure which contains prognostic equations for turbulent qu~tities, is used to study the physics and dynamics of ~ve~ion~ap~d marine strat~~~~ clouds. A set of numerical experiments had been performed to examined the role of sea surface temperature, huge-scale vertical velocity, wind speed, and vertical wind shear in the formation and the structure of low-level clouds. For a given sea surface and geostrophic wind speed, stratocumulus clouds can grow higher with smaller large-scale subsidence as less dry air entrains into the cloud. Clouds grow higher with higher sea surface temperature for a given geostrophic wind speed and large-scale subsidence as a result of enhanced moist convection. In high wind speeds, the entire cloud deck is lifted up because of larger surface energy flux. In the budget studies ofthe turbulent kinetic energy (TKE), the buoyancy term is a major source term when the wind speed and the vertical shear are small across the inversion top. When the wind speed and the vertical wind shear across the inversion top become large, the mixed layer is decoupled into a cloud and a subcloud layer. In the TKE budget studies, the shear generation term becomes an important term in the budgets of the TKE and the variance of vertical velocity." @default.
• W2576204857 created "2017-01-26" @default.
• W2576204857 creator A5024275401 @default.
• W2576204857 date "1987-01-01" @default.
• W2576204857 modified "2023-09-27" @default.
• W2576204857 title "A NUMERICAL STUDY OF THE MARINE STRATOCUMULUS CLOUD LAYER" @default.
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• W2576204857 hasPublicationYear "1987" @default.
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