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• W2160290429 abstract "The Surface Energy Balance Index is a normalized measure of relative evaporation based on relating observations of surface temperature to theoretical upper and lower bounds on the difference between surface and air temperature. More recently, the SEBI concept has been embedded in the Surface Energy Balance System (SEBS) by Su (2001, 2002). The reference height of air temperature is chosen to be representative of mean boundary layer over heterogeneous land surfaces. Observations of land surface temperature and shortwave reflectance are typically obtained by space- and airborne sensors. Estimates of latent and sensible heat flux density and of evaporative fraction may be obtained from SEBI – values. The paper summarizes results obtained in the context of validation experiments carried out in France, Italy, Spain, USA and China at local and regional spatial scales. At larger spatial scales, i.e. for the experiments in Spain, USA and China surface temperature and shortwave reflectance have been determined using the radiometric data obtained with AVHRR and the Along Track Scanning Radiometer (ATSR). To validate estimate of sensible heat flux density at larger spatial scales, extensive use of Large Aperture Scintillometers has been made. Agreement with observations was fair to good, notwithstanding the difficulty of estimating some SEBI parameters, such as the aerodynamic resistance for sensible heat transfer." @default.
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• W2160290429 date "2003-01-01" @default.
• W2160290429 modified "2023-09-26" @default.
• W2160290429 title "On SEBI-SEBS validation in France, Italy, Spain, USA and China" @default.
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