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    Indirect and Semi-direct Aerosol Campaign

    Source: Bulletin of the American Meteorological Society:;2010:;volume( 092 ):;issue: 002::page 183
    Author:
    McFarquhar, Greg M.
    ,
    Ghan, Steven
    ,
    Verlinde, Johannes
    ,
    Korolev, Alexei
    ,
    Strapp, J. Walter
    ,
    Schmid, Beat
    ,
    Tomlinson, Jason M.
    ,
    Wolde, Mengistu
    ,
    Brooks, Sarah D.
    ,
    Cziczo, Dan
    ,
    Dubey, Manvendra K.
    ,
    Fan, Jiwen
    ,
    Flynn, Connor
    ,
    Gultepe, Ismail
    ,
    Hubbe, John
    ,
    Gilles, Mary K.
    ,
    Laskin, Alexander
    ,
    Lawson, Paul
    ,
    Leaitch, W. Richard
    ,
    Liu, Peter
    ,
    Liu, Xiaohong
    ,
    Lubin, Dan
    ,
    Mazzoleni, Claudio
    ,
    Macdonald, Ann-Marie
    ,
    Moffet, Ryan C.
    ,
    Morrison, Hugh
    ,
    Ovchinnikov, Mikhail
    ,
    Shupe, Matthew D.
    ,
    Turner, David D.
    ,
    Xie, Shaocheng
    ,
    Zelenyuk, Alla
    ,
    Bae, Kenny
    ,
    Freer, Matt
    ,
    Glen, Andrew
    DOI: 10.1175/2010BAMS2935.1
    Publisher: American Meteorological Society
    Abstract: A comprehensive dataset of microphysical and radiative properties of aerosols and clouds in the boundary layer in the vicinity of Barrow, Alaska, was collected in April 2008 during the Indirect and Semi-Direct Aerosol Campaign (ISDAC). ISDAC's primary aim was to examine the effects of aerosols, including those generated by Asian wildfires, on clouds that contain both liquid and ice. ISDAC utilized the Atmospheric Radiation Measurement Pro- gram's permanent observational facilities at Barrow and specially deployed instruments measuring aerosol, ice fog, precipitation, and radiation. The National Research Council of Canada Convair-580 flew 27 sorties and collected data using an unprecedented 41 stateof- the-art cloud and aerosol instruments for more than 100 h on 12 different days. Aerosol compositions, including fresh and processed sea salt, biomassburning particles, organics, and sulfates mixed with organics, varied between flights. Observations in a dense arctic haze on 19 April and above, within, and below the single-layer stratocumulus on 8 and 26 April are enabling a process-oriented understanding of how aerosols affect arctic clouds. Inhomogeneities in reflectivity, a close coupling of upward and downward Doppler motion, and a nearly constant ice profile in the single-layer stratocumulus suggests that vertical mixing is responsible for its longevity observed during ISDAC. Data acquired in cirrus on flights between Barrow and Fairbanks, Alaska, are improving the understanding of the performance of cloud probes in ice. Ultimately, ISDAC data will improve the representation of cloud and aerosol processes in models covering a variety of spatial and temporal scales, and determine the extent to which surface measurements can provide retrievals of aerosols, clouds, precipitation, and radiative heating. A supplement to this article is available online: DOI: 10.1175/2010BAMS2935.2
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      Indirect and Semi-direct Aerosol Campaign

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4211567
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    contributor authorMcFarquhar, Greg M.
    contributor authorGhan, Steven
    contributor authorVerlinde, Johannes
    contributor authorKorolev, Alexei
    contributor authorStrapp, J. Walter
    contributor authorSchmid, Beat
    contributor authorTomlinson, Jason M.
    contributor authorWolde, Mengistu
    contributor authorBrooks, Sarah D.
    contributor authorCziczo, Dan
    contributor authorDubey, Manvendra K.
    contributor authorFan, Jiwen
    contributor authorFlynn, Connor
    contributor authorGultepe, Ismail
    contributor authorHubbe, John
    contributor authorGilles, Mary K.
    contributor authorLaskin, Alexander
    contributor authorLawson, Paul
    contributor authorLeaitch, W. Richard
    contributor authorLiu, Peter
    contributor authorLiu, Xiaohong
    contributor authorLubin, Dan
    contributor authorMazzoleni, Claudio
    contributor authorMacdonald, Ann-Marie
    contributor authorMoffet, Ryan C.
    contributor authorMorrison, Hugh
    contributor authorOvchinnikov, Mikhail
    contributor authorShupe, Matthew D.
    contributor authorTurner, David D.
    contributor authorXie, Shaocheng
    contributor authorZelenyuk, Alla
    contributor authorBae, Kenny
    contributor authorFreer, Matt
    contributor authorGlen, Andrew
    date accessioned2017-06-09T16:33:06Z
    date available2017-06-09T16:33:06Z
    date copyright2011/02/01
    date issued2010
    identifier issn0003-0007
    identifier otherams-69852.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4211567
    description abstractA comprehensive dataset of microphysical and radiative properties of aerosols and clouds in the boundary layer in the vicinity of Barrow, Alaska, was collected in April 2008 during the Indirect and Semi-Direct Aerosol Campaign (ISDAC). ISDAC's primary aim was to examine the effects of aerosols, including those generated by Asian wildfires, on clouds that contain both liquid and ice. ISDAC utilized the Atmospheric Radiation Measurement Pro- gram's permanent observational facilities at Barrow and specially deployed instruments measuring aerosol, ice fog, precipitation, and radiation. The National Research Council of Canada Convair-580 flew 27 sorties and collected data using an unprecedented 41 stateof- the-art cloud and aerosol instruments for more than 100 h on 12 different days. Aerosol compositions, including fresh and processed sea salt, biomassburning particles, organics, and sulfates mixed with organics, varied between flights. Observations in a dense arctic haze on 19 April and above, within, and below the single-layer stratocumulus on 8 and 26 April are enabling a process-oriented understanding of how aerosols affect arctic clouds. Inhomogeneities in reflectivity, a close coupling of upward and downward Doppler motion, and a nearly constant ice profile in the single-layer stratocumulus suggests that vertical mixing is responsible for its longevity observed during ISDAC. Data acquired in cirrus on flights between Barrow and Fairbanks, Alaska, are improving the understanding of the performance of cloud probes in ice. Ultimately, ISDAC data will improve the representation of cloud and aerosol processes in models covering a variety of spatial and temporal scales, and determine the extent to which surface measurements can provide retrievals of aerosols, clouds, precipitation, and radiative heating. A supplement to this article is available online: DOI: 10.1175/2010BAMS2935.2
    publisherAmerican Meteorological Society
    titleIndirect and Semi-direct Aerosol Campaign
    typeJournal Paper
    journal volume92
    journal issue2
    journal titleBulletin of the American Meteorological Society
    identifier doi10.1175/2010BAMS2935.1
    journal fristpage183
    journal lastpage201
    treeBulletin of the American Meteorological Society:;2010:;volume( 092 ):;issue: 002
    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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