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    Airmass Classification and Analysis of Aerosol Types at El Arenosillo (Spain)

    Source: Journal of Applied Meteorology and Climatology:;2009:;volume( 048 ):;issue: 005::page 962
    Author:
    Toledano, C.
    ,
    Cachorro, V. E.
    ,
    de Frutos, A. M.
    ,
    Torres, B.
    ,
    Berjón, A.
    ,
    Sorribas, M.
    ,
    Stone, R. S.
    DOI: 10.1175/2008JAMC2006.1
    Publisher: American Meteorological Society
    Abstract: The Aerosol Robotic Network (AERONET) site ?El Arenosillo,? equipped with a Cimel sun photometer, has been in operation since 2000. The data collected there are analyzed to establish an aerosol synoptic climatological description that is representative of the region. Different air masses and aerosol types are present over the site depending on the synoptic conditions. The frequent intrusion of dust from the Sahara Desert at El Arenosillo suggested the use of back trajectories to determine the airmass origins of other types of aerosol observed there. The focus of this study is to classify the air masses arriving at El Arenosillo by means of back-trajectory analyses and to characterize the aerosol within each type by means of the aerosol optical depth (AOD) and its spectral signature, given as the Ångström exponent (AE). The goal is to determine how aerosols observed over the station (receptor site) differ depending on source region and transport pathways. Two classification methods are used, one based on sectors and a second based on cluster analysis. The period analyzed is from 2000 to 2004. Both methods show that maritime air masses are predominant, occurring 70% of the time and having relatively low AOD (≈0.1 at 440 nm) and a wide range of AE (from about 0 to 2.0). Air masses with continental characteristics are moderately turbid and have values of AE that average ≈1.4. Air masses arriving from the south and southwest show the distinct features of the desert dust, having moderate to high values of AOD (0.30?0.35 at 440 nm) and low values of AE.
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      Airmass Classification and Analysis of Aerosol Types at El Arenosillo (Spain)

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4208091
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    • Journal of Applied Meteorology and Climatology

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    contributor authorToledano, C.
    contributor authorCachorro, V. E.
    contributor authorde Frutos, A. M.
    contributor authorTorres, B.
    contributor authorBerjón, A.
    contributor authorSorribas, M.
    contributor authorStone, R. S.
    date accessioned2017-06-09T16:22:33Z
    date available2017-06-09T16:22:33Z
    date copyright2009/05/01
    date issued2009
    identifier issn1558-8424
    identifier otherams-66723.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4208091
    description abstractThe Aerosol Robotic Network (AERONET) site ?El Arenosillo,? equipped with a Cimel sun photometer, has been in operation since 2000. The data collected there are analyzed to establish an aerosol synoptic climatological description that is representative of the region. Different air masses and aerosol types are present over the site depending on the synoptic conditions. The frequent intrusion of dust from the Sahara Desert at El Arenosillo suggested the use of back trajectories to determine the airmass origins of other types of aerosol observed there. The focus of this study is to classify the air masses arriving at El Arenosillo by means of back-trajectory analyses and to characterize the aerosol within each type by means of the aerosol optical depth (AOD) and its spectral signature, given as the Ångström exponent (AE). The goal is to determine how aerosols observed over the station (receptor site) differ depending on source region and transport pathways. Two classification methods are used, one based on sectors and a second based on cluster analysis. The period analyzed is from 2000 to 2004. Both methods show that maritime air masses are predominant, occurring 70% of the time and having relatively low AOD (≈0.1 at 440 nm) and a wide range of AE (from about 0 to 2.0). Air masses with continental characteristics are moderately turbid and have values of AE that average ≈1.4. Air masses arriving from the south and southwest show the distinct features of the desert dust, having moderate to high values of AOD (0.30?0.35 at 440 nm) and low values of AE.
    publisherAmerican Meteorological Society
    titleAirmass Classification and Analysis of Aerosol Types at El Arenosillo (Spain)
    typeJournal Paper
    journal volume48
    journal issue5
    journal titleJournal of Applied Meteorology and Climatology
    identifier doi10.1175/2008JAMC2006.1
    journal fristpage962
    journal lastpage981
    treeJournal of Applied Meteorology and Climatology:;2009:;volume( 048 ):;issue: 005
    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
    yabeshDSpacePersian