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 |
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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 |
format | Article |
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language | eng |
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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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