AbstractTwo different methods of computing regional evaporation from NOAA-AVHRR data are compared on a 250 × 250 km area for a particular day of the HAPEX-MOBILHY experiment. In the first one, the daily evaporation is linearly related to the surface temperature at 14h 00 UT ; in the other one, a simple planetary boundary layer model is used. The obtained differences are discussed, and a few improvements proposed.


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    Titel :

    Spatial integration of surface latent heat flux and evaporation mapping


    Beteiligte:
    Lagouarde, J.P. (Autor:in) / Brunet, Y. (Autor:in)

    Erschienen in:

    Erscheinungsdatum :

    01.01.1989


    Format / Umfang :

    6 pages




    Medientyp :

    Aufsatz (Zeitschrift)


    Format :

    Elektronische Ressource


    Sprache :

    Englisch



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