Show simple item record

contributor authorMcFarquhar, Greg M.
contributor authorUm, Junshik
contributor authorJackson, Robert
date accessioned2017-06-09T16:49:08Z
date available2017-06-09T16:49:08Z
date copyright2013/05/01
date issued2013
identifier issn1558-8424
identifier otherams-74694.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4216947
description abstracthe shapes of cloud particles with maximum dimensions Dmax between 35 and 60 ?m in mixed-phase clouds were studied using high-resolution particle images collected by a cloud particle imager (CPI) during the Mixed-Phase Arctic Cloud Experiment (M-PACE) and the Indirect and Semi-Direct Aerosol Campaign (ISDAC). The area ratio α, the projected area of a particle divided by the area of a circle with diameter Dmax, quantified particle shape. The differing optical characteristics of CPIs used in M-PACE and ISDAC had no effect on derived α provided that Dmax > 35 ?m and CPI focus > 45. The fraction of particles with 35 < Dmax < 60 ?m with α > 0.8 increased with the ratio of liquid water content (LWC) to total water content (TWC). The average αmean of small particles in each 10-s interval in mixed-phase clouds was correlated with LWC/TWC with a correlation coefficient of 0.60 for M-PACE and 0.43 for ISDAC. The stronger correlation seen during M-PACE was most likely associated with the presence of more liquid droplets that were larger than the CPI detection threshold contributing to αmean; the modal effective radius was larger (11 vs 6 ?m), and drops with D > 35 ?m had concentrations during M-PACE that were 6 times as large as those of ISDAC. This study hence suggests that area ratio can be used to identify the phase of particles with 35 < Dmax < 60 ?m and questions the assumption used in previous studies that all particles in this size range are supercooled droplets.
publisherAmerican Meteorological Society
titleSmall Cloud Particle Shapes in Mixed-Phase Clouds
typeJournal Paper
journal volume52
journal issue5
journal titleJournal of Applied Meteorology and Climatology
identifier doi10.1175/JAMC-D-12-0114.1
journal fristpage1277
journal lastpage1293
treeJournal of Applied Meteorology and Climatology:;2013:;volume( 052 ):;issue: 005
contenttypeFulltext


Files in this item

Thumbnail

This item appears in the following Collection(s)

Show simple item record