收稿：2019-10-21，
录用：2020-04-16，
纸质出版：2020-06-07
移动端阅览
Surface energy budget components (such as net radiation flux
sensible heat flux
latent heat flux and soil heat flux) at multiple temporal scales have significant meaning for understanding the energy and water cycle over the Tibetan Plateau (TP). In the framework of ESA-MOST Dragon Programme 4
the Surface Energy Balance System (SEBS) was tested and used to derive surface heat fluxes at different temporal scales over the TP by a combination use of geostationary satellite (FY-2C) data
polar orbiting satellite (SPOT/VGT
Terra/MODIS) data and ITPCAS forcing data. The validation results show there is a good agreement between derived heat fluxes and in situ measurements from Third Pole Environment Observation and Research
Platform (TPEORP)
which means the feasibility to derive surface heat fluxes over heterogeneous landscapes by a combination use of geostationary and polar orbiting satellite data in SEBS. The RMSEs for net radiation flux
sensible heat flux
latent heat flux and soil heat flux are 76.63 Wm
-2
60.29 Wm
-2
64.65 Wm
-2
and 37.5 Wm
-2
respectively. The diurnal
seasonal and inter-annual variation characteristics were also clearly identified through analyses of derived turbulent fluxes.
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