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    Longwave Radiation on Snow-Covered Mountainous Surfaces

    Source: Journal of Applied Meteorology:;1997:;volume( 036 ):;issue: 006::page 818
    Author:
    Plüss, Christian
    ,
    Ohmura, Atsumu
    DOI: 10.1175/1520-0450-36.6.818
    Publisher: American Meteorological Society
    Abstract: Longwave radiation in snow-covered alpine environments was investigated based on LOWTRAN7 calculations. The irradiance from the sky and from the surrounding topography were determined separately in order to detect the influence of the topography on longwave radiation balance. Sensitivity studies showed that the irradiance from the surrounding terrain is determined primarily by the atmospheric conditions within the investigated area and by the surface temperature of the surrounding terrain. In snow-covered environments, the air temperature is usually above the snow surface temperature and the effects of the air between the topography and the receiving surface may be relevant. Longwave irradiance from the surrounding terrain is an important component of the energy balance at the snow surface on inclined slopes and should be considered for areal investigations. A simple parameterization that accounts for the effects of the air is proposed for efficient calculation of longwave irradiance from snow-covered topography.
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      Longwave Radiation on Snow-Covered Mountainous Surfaces

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4148944
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    contributor authorPlüss, Christian
    contributor authorOhmura, Atsumu
    date accessioned2017-06-09T14:09:30Z
    date available2017-06-09T14:09:30Z
    date copyright1997/06/01
    date issued1997
    identifier issn0894-8763
    identifier otherams-13489.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4148944
    description abstractLongwave radiation in snow-covered alpine environments was investigated based on LOWTRAN7 calculations. The irradiance from the sky and from the surrounding topography were determined separately in order to detect the influence of the topography on longwave radiation balance. Sensitivity studies showed that the irradiance from the surrounding terrain is determined primarily by the atmospheric conditions within the investigated area and by the surface temperature of the surrounding terrain. In snow-covered environments, the air temperature is usually above the snow surface temperature and the effects of the air between the topography and the receiving surface may be relevant. Longwave irradiance from the surrounding terrain is an important component of the energy balance at the snow surface on inclined slopes and should be considered for areal investigations. A simple parameterization that accounts for the effects of the air is proposed for efficient calculation of longwave irradiance from snow-covered topography.
    publisherAmerican Meteorological Society
    titleLongwave Radiation on Snow-Covered Mountainous Surfaces
    typeJournal Paper
    journal volume36
    journal issue6
    journal titleJournal of Applied Meteorology
    identifier doi10.1175/1520-0450-36.6.818
    journal fristpage818
    journal lastpage824
    treeJournal of Applied Meteorology:;1997:;volume( 036 ):;issue: 006
    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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