During the Southern Great Plains experiment (SGP99), the electronically sca
nned thinned array radiometer (ESTAR) mapped L-band brightness temperature
over a swath about 50-km wide and 300 km long, extending west from Oklahoma
City, OK, to El Reno, OK, and north from the Little Washita River watershe
d to the Kansas border. ESTAR flew on the NASA P-3B Orion aircraft at an al
titude of 7.6 km, and maps were made on seven days between July 8-20, 1999.
The brightness temperature maps reflect the patterns of soil moisture expe
cted from rainfall and are consistent with values of soil moisture observed
at the research sites within the SGP99 study area and with previous measur
ements in this area. The data add to the resources for hydrologic modeling
in this area and are further validation of the technology represented by ES
TAR as a potential path to a future mission to map soil moisture globally f
rom space.