Remote Sensing Parameterization of Meso-scale Land Surface Evaporation

  • W. G. M. Bastiaanssen
  • M. Menenti
  • A. J. Dolman
  • R. A. Feddes
  • H. Pelgrum
Part of the Nato ASI Series book series (volume 45)


Land surface fluxes vary spatially as a result of the spatial heterogeneity of soil physical properties, fractional soil cover, land use, rainfall and hydrological processes. The scale at which this variability of surface fluxes occurs may be as low as a fraction of a meter, and time variations over a period of hours may be significant. The spatial average land surface flux at regional scale is because of length scale and sampling size difficult to quantify from field measurements. Although considerable progress has been made in this area over the last decade (e.g. Michand and Shuttleworth, 1996), there is no general consensus at this moment how to extrapolate surface fluxes from patch scale to meso-scale.


Heat Flux Land Surface Latent Heat Flux Surface Energy Balance Evaporative Fraction 
These keywords were added by machine and not by the authors. This process is experimental and the keywords may be updated as the learning algorithm improves.


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Copyright information

© Springer-Verlag Berlin Heidelberg 1996

Authors and Affiliations

  • W. G. M. Bastiaanssen
    • 1
  • M. Menenti
    • 1
  • A. J. Dolman
    • 1
  • R. A. Feddes
    • 1
  • H. Pelgrum
    • 1
  1. 1.Soil and Water ResearchDLO Winand Staring Centre for Integrated LandWageningenThe Netherlands

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