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    Eastern Pacific Emitted Aerosol Cloud Experiment

    Source: Bulletin of the American Meteorological Society:;2013:;volume( 094 ):;issue: 005::page 709
    Author:
    Russell, Lynn M.
    ,
    Sorooshian, Armin
    ,
    Seinfeld, John H.
    ,
    Albrecht, Bruce A.
    ,
    Nenes, Athanasios
    ,
    Ahlm, Lars
    ,
    Chen, Yi-Chun
    ,
    Coggon, Matthew
    ,
    Craven, Jill S.
    ,
    Flagan, Richard C.
    ,
    Frossard, Amanda A.
    ,
    Jonsson, Haflidi
    ,
    Jung, Eunsil
    ,
    Lin, Jack J.
    ,
    Metcalf, Andrew R.
    ,
    Modini, Robin
    ,
    Mülmenstädt, Johannes
    ,
    Roberts, Greg
    ,
    Shingler, Taylor
    ,
    Song, Siwon
    ,
    Wang, Zhen
    ,
    Wonaschütz, Anna
    DOI: 10.1175/BAMS-D-12-00015.1
    Publisher: American Meteorological Society
    Abstract: loud?radiation interactions are widely held to be the largest single source of uncertainty in climate model projections of future radiative forcing due to increasing anthropogenic emissions. The underlying causes of this uncertainty among modeled predictions of climate are the gaps in our fundamental understanding of cloud processes. There has been significant progress with both observations and models in addressing these important questions but quantifying them correctly is nontrivial, thus limiting our ability to represent them in global climate models. The Eastern Pacific Emitted Aerosol Cloud Experiment (E-PEACE) 2011 was a targeted aircraft campaign with embedded modeling studies, using the Center for Interdisciplinary Remotely-Piloted Aircraft Studies (CIRPAS) Twin Otter aircraft and the research vessel Point Sur in July and August 2011 off the central coast of California, with a full payload of instruments to measure particle and cloud number, mass, composition, and water uptake distributions. EPEACE used three emitted particle sources to separate particle-induced feedbacks from dynamical variability, namely 1) shipboard smoke-generated particles with 0.05?1-?m diameters (which produced tracks measured by satellite and had drop composition characteristic of organic smoke), 2) combustion particles from container ships with 0.05?0.2-?m diameters (which were measured in a variety of conditions with droplets containing both organic and sulfate components), and 3) aircraft-based milled salt particles with 3?5-?m diameters (which showed enhanced drizzle rates in some clouds). The aircraft observations were consistent with past large-eddy simulations of deeper clouds in ship tracks and aerosol? cloud parcel modeling of cloud drop number and composition, providing quantitative constraints on aerosol effects on warm-cloud microphysics.
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      Eastern Pacific Emitted Aerosol Cloud Experiment

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4215359
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    contributor authorRussell, Lynn M.
    contributor authorSorooshian, Armin
    contributor authorSeinfeld, John H.
    contributor authorAlbrecht, Bruce A.
    contributor authorNenes, Athanasios
    contributor authorAhlm, Lars
    contributor authorChen, Yi-Chun
    contributor authorCoggon, Matthew
    contributor authorCraven, Jill S.
    contributor authorFlagan, Richard C.
    contributor authorFrossard, Amanda A.
    contributor authorJonsson, Haflidi
    contributor authorJung, Eunsil
    contributor authorLin, Jack J.
    contributor authorMetcalf, Andrew R.
    contributor authorModini, Robin
    contributor authorMülmenstädt, Johannes
    contributor authorRoberts, Greg
    contributor authorShingler, Taylor
    contributor authorSong, Siwon
    contributor authorWang, Zhen
    contributor authorWonaschütz, Anna
    date accessioned2017-06-09T16:44:23Z
    date available2017-06-09T16:44:23Z
    date copyright2013/05/01
    date issued2013
    identifier issn0003-0007
    identifier otherams-73264.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4215359
    description abstractloud?radiation interactions are widely held to be the largest single source of uncertainty in climate model projections of future radiative forcing due to increasing anthropogenic emissions. The underlying causes of this uncertainty among modeled predictions of climate are the gaps in our fundamental understanding of cloud processes. There has been significant progress with both observations and models in addressing these important questions but quantifying them correctly is nontrivial, thus limiting our ability to represent them in global climate models. The Eastern Pacific Emitted Aerosol Cloud Experiment (E-PEACE) 2011 was a targeted aircraft campaign with embedded modeling studies, using the Center for Interdisciplinary Remotely-Piloted Aircraft Studies (CIRPAS) Twin Otter aircraft and the research vessel Point Sur in July and August 2011 off the central coast of California, with a full payload of instruments to measure particle and cloud number, mass, composition, and water uptake distributions. EPEACE used three emitted particle sources to separate particle-induced feedbacks from dynamical variability, namely 1) shipboard smoke-generated particles with 0.05?1-?m diameters (which produced tracks measured by satellite and had drop composition characteristic of organic smoke), 2) combustion particles from container ships with 0.05?0.2-?m diameters (which were measured in a variety of conditions with droplets containing both organic and sulfate components), and 3) aircraft-based milled salt particles with 3?5-?m diameters (which showed enhanced drizzle rates in some clouds). The aircraft observations were consistent with past large-eddy simulations of deeper clouds in ship tracks and aerosol? cloud parcel modeling of cloud drop number and composition, providing quantitative constraints on aerosol effects on warm-cloud microphysics.
    publisherAmerican Meteorological Society
    titleEastern Pacific Emitted Aerosol Cloud Experiment
    typeJournal Paper
    journal volume94
    journal issue5
    journal titleBulletin of the American Meteorological Society
    identifier doi10.1175/BAMS-D-12-00015.1
    journal fristpage709
    journal lastpage729
    treeBulletin of the American Meteorological Society:;2013:;volume( 094 ):;issue: 005
    contenttypeFulltext
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    DSpace software copyright © 2002-2015  DuraSpace
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