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contributor authorSchwiesow, R. L.
contributor authorMayor, S. D.
contributor authorGlover, V. M.
contributor authorLenschow, D. H.
date accessioned2017-06-09T14:03:16Z
date available2017-06-09T14:03:16Z
date copyright1990/11/01
date issued1990
identifier issn0894-8763
identifier otherams-11616.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4146864
description abstractThe NCAR Airborne Infrared Lidar System (NAILS) observed the edge of an extended, sloping aerosol layer that intersected a stratocumulus cloud deck over the Pacific Ocean during the First ISCCP (International Satellite Cloud Climatology Project) Regional Experiment, 260 km WNW of San Diego. In situ measurements support the interpretation of the lidar observations as arising from a particle-laden layer with relatively clean air above, below, and to the SW. Intersection of these sloping layers with cloud top leads to substantial horizontal variability of boundary-layer structure in the intersection region. The intersection of the aerosol layer with cloud top also corresponded closely to a quasi-linear trough in the cloud top that showed enhanced brightness and an enhanced number of small particles.
publisherAmerican Meteorological Society
titleIntersection of a Sloping Aerosol Layer Observed by Airborne Lidar with a Cloud-Capped Marine Boundary Layer
typeJournal Paper
journal volume29
journal issue11
journal titleJournal of Applied Meteorology
identifier doi10.1175/1520-0450(1990)029<1111:IOASAL>2.0.CO;2
journal fristpage1111
journal lastpage1119
treeJournal of Applied Meteorology:;1990:;volume( 029 ):;issue: 011
contenttypeFulltext


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