Generation of a 3-years time serie of daily actual evapotranspiration over the Tibetan Plateau

摘要

The estimation of turbulent u001fuxes is of primary interest for hydrological andrnclimatological studies. Also the use of optical remote sensing data in the VNIR and TIRrndomain already proved to allow for the parameterization of surface energy balance,rnleading to many algorithms. Their use over arid high elevation areas require detailedrncharacterisation of key surface physical properties and atmospheric statement at arnreference level. Satellite products aquired over the Tibetan Plateau and simulationsrnresults delivered in the frame of the CEOP-AEGIS project provide incentives for a regularrnanalysis at medium scale.