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    Effects of Sahel Dust Layers upon Nocturnal Cooling of the Atmosphere (ECLATS Experiment)

    Source: Journal of Climate and Applied Meteorology:;1984:;volume( 023 ):;issue: 004::page 644
    Author:
    Guedalia, Daniel
    ,
    Estournel, Claude
    ,
    Vehil, Raoul
    DOI: 10.1175/1520-0450(1984)023<0644:EOSDLU>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: A study of the effect of a desert aerosol layer on the nocturnal cooling of the atmosphere is presented. The experimental data were obtained during the ECLATS experiment which was run in the Sahel region of the Niger in November 1980. This study uses measurements of thermodynamic and radiative parameters, aerosol size distribution, and a radiative model. The results show that the presence of a dust layer at night increases the downward infrared flux at the surface (and then modifies the energy budget) and increases the radiative cooling rate of the atmosphere, slightly in the layers near the ground (?0.15 K h?1) and in a more important way at the top of the haze layer.
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      Effects of Sahel Dust Layers upon Nocturnal Cooling of the Atmosphere (ECLATS Experiment)

    URI
    http://yetl.yabesh.ir/yetl1/handle/yetl/4145850
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    • Journal of Climate and Applied Meteorology

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    contributor authorGuedalia, Daniel
    contributor authorEstournel, Claude
    contributor authorVehil, Raoul
    date accessioned2017-06-09T14:00:08Z
    date available2017-06-09T14:00:08Z
    date copyright1984/04/01
    date issued1984
    identifier issn0733-3021
    identifier otherams-10703.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4145850
    description abstractA study of the effect of a desert aerosol layer on the nocturnal cooling of the atmosphere is presented. The experimental data were obtained during the ECLATS experiment which was run in the Sahel region of the Niger in November 1980. This study uses measurements of thermodynamic and radiative parameters, aerosol size distribution, and a radiative model. The results show that the presence of a dust layer at night increases the downward infrared flux at the surface (and then modifies the energy budget) and increases the radiative cooling rate of the atmosphere, slightly in the layers near the ground (?0.15 K h?1) and in a more important way at the top of the haze layer.
    publisherAmerican Meteorological Society
    titleEffects of Sahel Dust Layers upon Nocturnal Cooling of the Atmosphere (ECLATS Experiment)
    typeJournal Paper
    journal volume23
    journal issue4
    journal titleJournal of Climate and Applied Meteorology
    identifier doi10.1175/1520-0450(1984)023<0644:EOSDLU>2.0.CO;2
    journal fristpage644
    journal lastpage650
    treeJournal of Climate and Applied Meteorology:;1984:;volume( 023 ):;issue: 004
    contenttypeFulltext
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    DSpace software copyright © 2002-2015  DuraSpace
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