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contributor authorde Boer, Gijs
contributor authorEloranta, Edwin W.
contributor authorShupe, Matthew D.
date accessioned2017-06-09T16:28:16Z
date available2017-06-09T16:28:16Z
date copyright2009/09/01
date issued2009
identifier issn0022-4928
identifier otherams-68461.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4210021
description abstractMacro- and microphysical properties of single-layer stratiform mixed-phase clouds are derived from multiple years of lidar, radar, and radiosonde observations. Measurements were made as part of the Mixed-Phase Arctic Clouds Experiment (MPACE) and the Study of Environmental Arctic Change (SEARCH) in Barrow, Alaska, and Eureka, Nunavut, Canada, respectively. Single-layer mixed-phase clouds occurred between 4% and 26% of the total time observed, varying with season and location. They had mean cloud-base heights between ?700 and 2100 m and thicknesses between ?200 and 700 m. Seasonal mean cloud optical depths ranged from 2.2 up. The clouds existed at temperatures of ?242?271 K and occurred under different wind conditions, depending on season. Utilizing retrievals from a combination of lidar, radar, and microwave radiometer, mean cloud microphysical properties were derived, with mean liquid effective diameters estimated from 16 to 49 ?m, mean liquid number densities on the order of 104?105 L?1, and mean water contents estimated between 0.07 and 0.28 g m?3. Ice precipitation was shown to have mean ice effective diameters of 50?125 ?m, mean ice number densities on the order of 10 L?1, and mean water contents estimated between 0.012 and 0.031 g m?3. Mean cloud liquid water paths ranged from 25 to 100 g m?2. All results are compared to previous studies, and potential retrieval errors are discussed. Additionally, seasonal variation in macro- and microphysical properties was highlighted. Finally, fraction of liquid water to ice mass was shown to decrease with decreasing temperature.
publisherAmerican Meteorological Society
titleArctic Mixed-Phase Stratiform Cloud Properties from Multiple Years of Surface-Based Measurements at Two High-Latitude Locations
typeJournal Paper
journal volume66
journal issue9
journal titleJournal of the Atmospheric Sciences
identifier doi10.1175/2009JAS3029.1
journal fristpage2874
journal lastpage2887
treeJournal of the Atmospheric Sciences:;2009:;Volume( 066 ):;issue: 009
contenttypeFulltext


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