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    The Midlatitude Continental Convective Clouds Experiment (MC3E)

    Source: Bulletin of the American Meteorological Society:;2015:;volume( 097 ):;issue: 009::page 1667
    Author:
    Jensen, M. P.
    ,
    Petersen, W. A.
    ,
    Bansemer, A.
    ,
    Bharadwaj, N.
    ,
    Carey, L. D.
    ,
    Cecil, D. J.
    ,
    Collis, S. M.
    ,
    Del Genio, A. D.
    ,
    Dolan, B.
    ,
    Gerlach, J.
    ,
    Giangrande, S. E.
    ,
    Heymsfield, A.
    ,
    Heymsfield, G.
    ,
    Kollias, P.
    ,
    Lang, T. J.
    ,
    Nesbitt, S. W.
    ,
    Neumann, A.
    ,
    Poellot, M.
    ,
    Rutledge, S. A.
    ,
    Schwaller, M.
    ,
    Tokay, A.
    ,
    Williams, C. R.
    ,
    Wolff, D. B.
    ,
    Xie, S.
    ,
    Zipser, E. J.
    DOI: 10.1175/BAMS-D-14-00228.1
    Publisher: American Meteorological Society
    Abstract: he Midlatitude Continental Convective Clouds Experiment (MC3E), a field program jointly led by the U.S. Department of Energy?s Atmospheric Radiation Measurement (ARM) Program and the National Aeronautics and Space Administration?s (NASA) Global Precipitation Measurement (GPM) mission, was conducted in south-central Oklahoma during April?May 2011. MC3E science objectives were motivated by the need to improve our understanding of midlatitude continental convective cloud system life cycles, microphysics, and GPM precipitation retrieval algorithms. To achieve these objectives, a multiscale surface- and aircraft-based in situ and remote sensing observing strategy was employed. A variety of cloud and precipitation events were sampled during MC3E, of which results from three deep convective events are highlighted. Vertical structure, air motions, precipitation drop size distributions, and ice properties were retrieved from multiwavelength radar, profiler, and aircraft observations for a mesoscale convective system (MCS) on 11 May. Aircraft observations for another MCS observed on 20 May were used to test agreement between observed radar reflectivities and those calculated with forward-modeled reflectivity and microwave brightness temperatures using in situ particle size distributions and ice water content. Multiplatform observations of a supercell that occurred on 23 May allowed for an integrated analysis of kinematic and microphysical interactions. A core updraft of 25 m s?1 supported growth of hail and large raindrops. Data collected during the MC3E campaign are being used in a number of current and ongoing research projects and are available through the ARM and NASA data archives.
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      The Midlatitude Continental Convective Clouds Experiment (MC3E)

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4215759
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    • Bulletin of the American Meteorological Society

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    contributor authorJensen, M. P.
    contributor authorPetersen, W. A.
    contributor authorBansemer, A.
    contributor authorBharadwaj, N.
    contributor authorCarey, L. D.
    contributor authorCecil, D. J.
    contributor authorCollis, S. M.
    contributor authorDel Genio, A. D.
    contributor authorDolan, B.
    contributor authorGerlach, J.
    contributor authorGiangrande, S. E.
    contributor authorHeymsfield, A.
    contributor authorHeymsfield, G.
    contributor authorKollias, P.
    contributor authorLang, T. J.
    contributor authorNesbitt, S. W.
    contributor authorNeumann, A.
    contributor authorPoellot, M.
    contributor authorRutledge, S. A.
    contributor authorSchwaller, M.
    contributor authorTokay, A.
    contributor authorWilliams, C. R.
    contributor authorWolff, D. B.
    contributor authorXie, S.
    contributor authorZipser, E. J.
    date accessioned2017-06-09T16:45:40Z
    date available2017-06-09T16:45:40Z
    date copyright2016/09/01
    date issued2015
    identifier issn0003-0007
    identifier otherams-73624.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4215759
    description abstracthe Midlatitude Continental Convective Clouds Experiment (MC3E), a field program jointly led by the U.S. Department of Energy?s Atmospheric Radiation Measurement (ARM) Program and the National Aeronautics and Space Administration?s (NASA) Global Precipitation Measurement (GPM) mission, was conducted in south-central Oklahoma during April?May 2011. MC3E science objectives were motivated by the need to improve our understanding of midlatitude continental convective cloud system life cycles, microphysics, and GPM precipitation retrieval algorithms. To achieve these objectives, a multiscale surface- and aircraft-based in situ and remote sensing observing strategy was employed. A variety of cloud and precipitation events were sampled during MC3E, of which results from three deep convective events are highlighted. Vertical structure, air motions, precipitation drop size distributions, and ice properties were retrieved from multiwavelength radar, profiler, and aircraft observations for a mesoscale convective system (MCS) on 11 May. Aircraft observations for another MCS observed on 20 May were used to test agreement between observed radar reflectivities and those calculated with forward-modeled reflectivity and microwave brightness temperatures using in situ particle size distributions and ice water content. Multiplatform observations of a supercell that occurred on 23 May allowed for an integrated analysis of kinematic and microphysical interactions. A core updraft of 25 m s?1 supported growth of hail and large raindrops. Data collected during the MC3E campaign are being used in a number of current and ongoing research projects and are available through the ARM and NASA data archives.
    publisherAmerican Meteorological Society
    titleThe Midlatitude Continental Convective Clouds Experiment (MC3E)
    typeJournal Paper
    journal volume97
    journal issue9
    journal titleBulletin of the American Meteorological Society
    identifier doi10.1175/BAMS-D-14-00228.1
    journal fristpage1667
    journal lastpage1686
    treeBulletin of the American Meteorological Society:;2015:;volume( 097 ):;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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