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    Influence of Rainfall on the Seasonal Variations of Cloud Condensation Nuclei Concentrations in a Sub-Equatorial Climate

    Source: Journal of the Atmospheric Sciences:;1982:;Volume( 039 ):;issue: 009::page 2076
    Author:
    Désalmand, F.
    ,
    Baudet, J.
    ,
    Serpolay, R.
    DOI: 10.1175/1520-0469(1982)039<2076:IOROTS>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Systematic measurements of cloud condensation nuclei (CCN) concentration have been carried out in the Abidjan area from December 1977 to June 1978, at 0700 local time (corresponding to a daily maximum). In that period of the year, from the main dry season to the main rainy season, a general decrease of CCN concentrations has been noted. This decrease is more marked for the more active CCN. In May and June 1978, during the continuous monsoon rains, the concentrations substantially increased, this effect being more important for the fraction of the less active CCN. Nuclei of continental origin accompanying dust haze in December 1977 were progressively eliminated from the atmosphere by dry or wet deposition. They wore replaced by smaller nuclei. originating in vegetation, the production of which was increased by the continuous monsoon rains.
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      Influence of Rainfall on the Seasonal Variations of Cloud Condensation Nuclei Concentrations in a Sub-Equatorial Climate

    URI
    http://yetl.yabesh.ir/yetl1/handle/yetl/4154421
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    • Journal of the Atmospheric Sciences

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    contributor authorDésalmand, F.
    contributor authorBaudet, J.
    contributor authorSerpolay, R.
    date accessioned2017-06-09T14:23:21Z
    date available2017-06-09T14:23:21Z
    date copyright1982/09/01
    date issued1982
    identifier issn0022-4928
    identifier otherams-18418.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4154421
    description abstractSystematic measurements of cloud condensation nuclei (CCN) concentration have been carried out in the Abidjan area from December 1977 to June 1978, at 0700 local time (corresponding to a daily maximum). In that period of the year, from the main dry season to the main rainy season, a general decrease of CCN concentrations has been noted. This decrease is more marked for the more active CCN. In May and June 1978, during the continuous monsoon rains, the concentrations substantially increased, this effect being more important for the fraction of the less active CCN. Nuclei of continental origin accompanying dust haze in December 1977 were progressively eliminated from the atmosphere by dry or wet deposition. They wore replaced by smaller nuclei. originating in vegetation, the production of which was increased by the continuous monsoon rains.
    publisherAmerican Meteorological Society
    titleInfluence of Rainfall on the Seasonal Variations of Cloud Condensation Nuclei Concentrations in a Sub-Equatorial Climate
    typeJournal Paper
    journal volume39
    journal issue9
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/1520-0469(1982)039<2076:IOROTS>2.0.CO;2
    journal fristpage2076
    journal lastpage2082
    treeJournal of the Atmospheric Sciences:;1982:;Volume( 039 ):;issue: 009
    contenttypeFulltext
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