Show simple item record

contributor authorHudson, James G.
contributor authorSvensson, Gunilla
date accessioned2017-06-09T14:05:31Z
date available2017-06-09T14:05:31Z
date copyright1995/12/01
date issued1995
identifier issn0894-8763
identifier otherams-12244.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4147562
description abstractCloud microphysical measurements off the southern California coast are presented and compared with in situ airborne measurements of cloud condensation nuclei (CCN) spectra. Large-scale variations in cloud droplet concentrations were due to CCN variations, some medium-scale variations may be a result of the conversion of droplets to drops by coalescence, while small-scale variations were due to different proportions of the CCN spectra being activated because of variations in updraft velocity at cloud base. This latter internal mixing process produces an inverse relationship between droplet concentration and mean size and an increase in droplet spectral width with mean droplet size. Drizzle drop concentrations are strongly associated with lower droplet concentrations, larger droplets, and greater droplet spectral width.
publisherAmerican Meteorological Society
titleCloud Microphysical Relationships in California Marine Stratus
typeJournal Paper
journal volume34
journal issue12
journal titleJournal of Applied Meteorology
identifier doi10.1175/1520-0450(1995)034<2655:CMRICM>2.0.CO;2
journal fristpage2655
journal lastpage2666
treeJournal of Applied Meteorology:;1995:;volume( 034 ):;issue: 012
contenttypeFulltext


Files in this item

Thumbnail

This item appears in the following Collection(s)

Show simple item record