Diurnal Evolution of the Cloud-Topped Marine Boundary Layer. Part I: Nocturnal Stratocumulus Development

In the Atlantic Stratocumulus Transition Experiment, aircraft measurements show a surface-based mixed layer separated from the base of the stratocumulus by a layer that is stable to dry turbulent mixing. This layer forms due to shortwave heating of the stratocumulus clouds.

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Veröffentlicht in:Journal of the atmospheric sciences 1995-08, Vol.52 (16), p.2953-2966
Hauptverfasser: Rogers, David P, Yang, Xiaohua, Norris, Peter M, Johnson, Douglas W
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container_title Journal of the atmospheric sciences
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creator Rogers, David P
Yang, Xiaohua
Norris, Peter M
Johnson, Douglas W
description In the Atlantic Stratocumulus Transition Experiment, aircraft measurements show a surface-based mixed layer separated from the base of the stratocumulus by a layer that is stable to dry turbulent mixing. This layer forms due to shortwave heating of the stratocumulus clouds.
doi_str_mv 10.1175/1520-0469(1995)052<2953:DEOTCT>2.0.CO;2
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source American Meteorological Society; EZB-FREE-00999 freely available EZB journals; Alma/SFX Local Collection
subjects Atmosphere
Boundary layers
Clouds
Meteorology
title Diurnal Evolution of the Cloud-Topped Marine Boundary Layer. Part I: Nocturnal Stratocumulus Development
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