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    The Change in Earth-Atmosphere Albedo and Radiational Equilibrium Temperatures due to Stratospheric Pollution

    Source: Journal of Applied Meteorology:;1976:;volume( 015 ):;issue: 010::page 1057
    Author:
    Herman, Benjamin M.
    ,
    Browning, S. Robert
    ,
    Rabinoff, Robert
    DOI: 10.1175/1520-0450(1976)015<1057:TCIEAA>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: The changes in the earth-atmosphere albedo and radiative equilibrium temperature due to perturbations in the solar radiative balance are investigated. The perturbations are induced through the introduction of varying amounts of aerosols into the stratospheric layer between 15 and 25 km. Results are presented graphically as a function of latitude and season for a range of aerosol absorption coefficients and for a specific aerosol composed of a 75% sulphuric acid solution. These results indicate that such aerosol perturbations on the solar energy field result in larger albedo and radiative equilibrium changes in polar latitudes than in middle or tropical latitudes.
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      The Change in Earth-Atmosphere Albedo and Radiational Equilibrium Temperatures due to Stratospheric Pollution

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4232612
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    • Journal of Applied Meteorology

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    contributor authorHerman, Benjamin M.
    contributor authorBrowning, S. Robert
    contributor authorRabinoff, Robert
    date accessioned2017-06-09T17:38:46Z
    date available2017-06-09T17:38:46Z
    date copyright1976/10/01
    date issued1976
    identifier issn0021-8952
    identifier otherams-9155.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4232612
    description abstractThe changes in the earth-atmosphere albedo and radiative equilibrium temperature due to perturbations in the solar radiative balance are investigated. The perturbations are induced through the introduction of varying amounts of aerosols into the stratospheric layer between 15 and 25 km. Results are presented graphically as a function of latitude and season for a range of aerosol absorption coefficients and for a specific aerosol composed of a 75% sulphuric acid solution. These results indicate that such aerosol perturbations on the solar energy field result in larger albedo and radiative equilibrium changes in polar latitudes than in middle or tropical latitudes.
    publisherAmerican Meteorological Society
    titleThe Change in Earth-Atmosphere Albedo and Radiational Equilibrium Temperatures due to Stratospheric Pollution
    typeJournal Paper
    journal volume15
    journal issue10
    journal titleJournal of Applied Meteorology
    identifier doi10.1175/1520-0450(1976)015<1057:TCIEAA>2.0.CO;2
    journal fristpage1057
    journal lastpage1067
    treeJournal of Applied Meteorology:;1976:;volume( 015 ):;issue: 010
    contenttypeFulltext
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    DSpace software copyright © 2002-2015  DuraSpace
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