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    Incident Solar Radiation over Europe Estimated from METEOSAT Data

    Source: Journal of Climate and Applied Meteorology:;1984:;volume( 023 ):;issue: 001::page 166
    Author:
    Möser, Werner
    ,
    Raschke, Ehrhard
    DOI: 10.1175/1520-0450(1984)023<0166:ISROEE>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Daily sums of the downward solar radiation, i.e., the global radiation, have been computed from imaging data of reflected solar and emitted infrared radiation which were measured from the geostationary satellites METEOSAT I and II during the periods 1-30 June 1979 and 1-30 April 1982, respectively, over Europe and northern Africa. The method assumes basically that clouds perturb the ?clear sky? radiance fields. Thus, the satellite data of reflected solar radiation are used as indicators for the presence of clouds and of their transparency for radiation scattered upward from underneath. Radiative transfer calculations have been employed to determine clouds and atmospheric transmittance for solar radiation at different zenith angles. A comparison with simultaneous measurements of the European network of pyranometers yields rms differences of 0.25 kWh m?2 (June 1979) and 0.28 kWh m?2 (April 1982), respectively, for monthly averages of daily sums. This uncertainty corresponds to ?5?6% of the available insolation. Our results are available with a resolution of about 25?25 km2.
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      Incident Solar Radiation over Europe Estimated from METEOSAT Data

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4145792
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    contributor authorMöser, Werner
    contributor authorRaschke, Ehrhard
    date accessioned2017-06-09T13:59:57Z
    date available2017-06-09T13:59:57Z
    date copyright1984/01/01
    date issued1984
    identifier issn0733-3021
    identifier otherams-10651.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4145792
    description abstractDaily sums of the downward solar radiation, i.e., the global radiation, have been computed from imaging data of reflected solar and emitted infrared radiation which were measured from the geostationary satellites METEOSAT I and II during the periods 1-30 June 1979 and 1-30 April 1982, respectively, over Europe and northern Africa. The method assumes basically that clouds perturb the ?clear sky? radiance fields. Thus, the satellite data of reflected solar radiation are used as indicators for the presence of clouds and of their transparency for radiation scattered upward from underneath. Radiative transfer calculations have been employed to determine clouds and atmospheric transmittance for solar radiation at different zenith angles. A comparison with simultaneous measurements of the European network of pyranometers yields rms differences of 0.25 kWh m?2 (June 1979) and 0.28 kWh m?2 (April 1982), respectively, for monthly averages of daily sums. This uncertainty corresponds to ?5?6% of the available insolation. Our results are available with a resolution of about 25?25 km2.
    publisherAmerican Meteorological Society
    titleIncident Solar Radiation over Europe Estimated from METEOSAT Data
    typeJournal Paper
    journal volume23
    journal issue1
    journal titleJournal of Climate and Applied Meteorology
    identifier doi10.1175/1520-0450(1984)023<0166:ISROEE>2.0.CO;2
    journal fristpage166
    journal lastpage170
    treeJournal of Climate and Applied Meteorology:;1984:;volume( 023 ):;issue: 001
    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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