Gr. Diak et al., REMOTE-SENSING OF LAND-SURFACE ENERGY-BALANCE USING DATA FROM THE HIGH-RESOLUTION INTERFEROMETER SOUNDER (HIS) - A SIMULATION STUDY, Remote sensing of environment, 48(1), 1994, pp. 106-118
The remote sensing of the land-surface energy balance and soil moistur
e using satellite surface 'skin' temperature measurements has long bee
n a topic of investigation in the research community. Despite consider
able progress in understanding and techniques, there are still serious
limitations in the results obtainable using satellite measurements fo
r both the surface fluxes and soil moisture which need to be addressed
via improved measurements and methods. We detail in this work a simul
ation study investigating the remote sensing of the land-surface energ
y balance using information from the High-resolution Interferometer So
under (HIS), an instrument being considered for launch on a future ser
ies of geostationary satellites. The study is accomplished using simul
ated HIS data that are generated using atmospheric radiative transfer
models specific to the HIS applied to the output of a forecast model o
f the planetary boundary layer, which predicts temporal changes in ski
n temperature and atmospheric structure based on the surface fluxes. I
n this study, we find that the ability of the instrument to measure te
mporal changes of radiances that arise from time changes in the struct
ure of the planetary boundary layer, as well as skin temperature chang
es, mitigates some Of the problems associated with using skin temperat
ures alone to estimate the surface energy balance.