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    Arctic Mixed-Phase Stratiform Cloud Properties from Multiple Years of Surface-Based Measurements at Two High-Latitude Locations

    Source: Journal of the Atmospheric Sciences:;2009:;Volume( 066 ):;issue: 009::page 2874
    Author:
    de Boer, Gijs
    ,
    Eloranta, Edwin W.
    ,
    Shupe, Matthew D.
    DOI: 10.1175/2009JAS3029.1
    Publisher: American Meteorological Society
    Abstract: Macro- 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.
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      Arctic Mixed-Phase Stratiform Cloud Properties from Multiple Years of Surface-Based Measurements at Two High-Latitude Locations

    URI
    http://yetl.yabesh.ir/yetl1/handle/yetl/4210021
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    • Journal of the Atmospheric Sciences

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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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    DSpace software copyright © 2002-2015  DuraSpace
    نرم افزار کتابخانه دیجیتال "دی اسپیس" فارسی شده توسط یابش برای کتابخانه های ایرانی | تماس با یابش
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