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    The Temperature of Evaporating Sea Spray Droplets

    Source: Journal of the Atmospheric Sciences:;1995:;Volume( 052 ):;issue: 007::page 852
    Author:
    Andreas, Edgar L.
    DOI: 10.1175/1520-0469(1995)052<0852:TTOESS>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Evaporating sea spray droplets are often assumed to be at the temperature of a well-ventilated wet-bulb thermometer, Twet. Although this assumption may be accurate enough in practice, it is incorrect on theoretical grounds. Spray droplets have curved surfaces, they contain dissolved salts, and they may be small enough that the air and water vapor surrounding them do not behave as continuous fluids. Each of these characteristics of aqueous solution droplets can potentially affect vapor exchange at a droplet's surface and, thus, its temperature; but the wet-bulb temperature accounts for none of these. This paper uses a full microphysical model to accurately predict the evaporating temperature, Tev, of pure and saline droplets to investigate how close Twet is to this temperature. In general, Twet is within ?0.2°?0,3°C of Tev for droplets with salinities from 0 to 40 psu when the droplet radius is 10 µm or greater. When the droplet radius is less than 10 ?m, however. Twet can underestimate Tev badly, especially for higher air temperatures. To provide accurate estimates of Tev quickly, the paper describes an algorithm that predicts Tev to within 0.3°C of the temperature predicted by the full model for droplets with radii from 0.5 to 500 µm when air temperatures are from ?10° to 30°C, relative humidities am from 80% to 97.5%, and droplet salinities are from 0 to 40 psu.
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      The Temperature of Evaporating Sea Spray Droplets

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    contributor authorAndreas, Edgar L.
    date accessioned2017-06-09T14:32:54Z
    date available2017-06-09T14:32:54Z
    date copyright1995/04/01
    date issued1995
    identifier issn0022-4928
    identifier otherams-21410.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4157747
    description abstractEvaporating sea spray droplets are often assumed to be at the temperature of a well-ventilated wet-bulb thermometer, Twet. Although this assumption may be accurate enough in practice, it is incorrect on theoretical grounds. Spray droplets have curved surfaces, they contain dissolved salts, and they may be small enough that the air and water vapor surrounding them do not behave as continuous fluids. Each of these characteristics of aqueous solution droplets can potentially affect vapor exchange at a droplet's surface and, thus, its temperature; but the wet-bulb temperature accounts for none of these. This paper uses a full microphysical model to accurately predict the evaporating temperature, Tev, of pure and saline droplets to investigate how close Twet is to this temperature. In general, Twet is within ?0.2°?0,3°C of Tev for droplets with salinities from 0 to 40 psu when the droplet radius is 10 µm or greater. When the droplet radius is less than 10 ?m, however. Twet can underestimate Tev badly, especially for higher air temperatures. To provide accurate estimates of Tev quickly, the paper describes an algorithm that predicts Tev to within 0.3°C of the temperature predicted by the full model for droplets with radii from 0.5 to 500 µm when air temperatures are from ?10° to 30°C, relative humidities am from 80% to 97.5%, and droplet salinities are from 0 to 40 psu.
    publisherAmerican Meteorological Society
    titleThe Temperature of Evaporating Sea Spray Droplets
    typeJournal Paper
    journal volume52
    journal issue7
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/1520-0469(1995)052<0852:TTOESS>2.0.CO;2
    journal fristpage852
    journal lastpage862
    treeJournal of the Atmospheric Sciences:;1995:;Volume( 052 ):;issue: 007
    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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