Abstract
Abstract A simple physically-based method for estimating the daily surface outgoing longwave radiative flux during cloudless days is presented. The proposed algorithm is well-suited for remote sensing purposes, in the framework of surface net radiation and evapotranspiration studies: it only requires the NOAA-AVHRR derived surface temperature acquired in the early afternoon, the minimum air temperature easily obtainable from the meteorological network, and the day-length computed from the site coordinates and the date. The algorithm features one single empirical coefficient, adjusted statistically on a large data set generated by a coupled heat and mass transfer model between the soil and the atmosphere. The method is then validated against ten different experimental data sets, covering a wide range of surface, climate and weather conditions. The validation is performed at the daily and five-day scales and is shown to lead to a good precision. The sources of errors are then discussed and a map of the surf...
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Disclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.