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8 November 2014Evaluation of the harmonic-analysis method for surface soil heat flux estimation: a case study in Heihe River Basin
Surface soil heat flux(G0) is an important component of surface energy balance, and it causes large uncertainty in
evapotranspiration estimation. In present study, soil heat flux was calculated at different depths based on the harmonic
analysis method (HM) using field data in Heihe River Basin, northwestern China. The soil heat fluxes at a certain depth
and at the surface were validated by heat-plate measurements and G0 derived from thermal diffusion equation,
respectively. Results showed that HM method obtained good result during the daytime, yet the errors were relatively
large at nighttime mostly due to the assumption of symmetry of G0 during daytime and nighttime. Moreover, a regional
G0 map was provided based on remote sensing data. This study highlighted the simplicity of HM method and its
potential application in large spatial scale mapping. Its internal limit was also discussed here.
Nana Li,Li Jia, andChaolei Zheng
"Evaluation of the harmonic-analysis method for surface soil heat flux estimation: a case study in Heihe River Basin", Proc. SPIE 9260, Land Surface Remote Sensing II, 926043 (8 November 2014); https://doi.org/10.1117/12.2069270
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Nana Li, Li Jia, Chaolei Zheng, "Evaluation of the harmonic-analysis method for surface soil heat flux estimation: a case study in Heihe River Basin," Proc. SPIE 9260, Land Surface Remote Sensing II, 926043 (8 November 2014); https://doi.org/10.1117/12.2069270