Jr. Wang, SOME FEATURES OBSERVED BY THE L-BAND PUSH BROOM MICROWAVE RADIOMETER OVER THE KONZA PRAIRIE DURING 1985-1989, JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 100(D12), 1995, pp. 25469-25479
Airborne L-band radiometric measurements were conducted over the Konza
Prairie near Manhattan, Kansas, in the summers of 1985, 1987, 1988, a
nd 1989 to study the relationship among surface microwave emission, so
il moisture, and vegetation cover. The annual surface treatments that
were applied to the watersheds in the experimental area appeared to sh
ow a significant impact on the surface microwave emission. A watershed
that was burned every year showed a better sensitivity to soil moistu
re variation than those burned less frequently. This feature persisted
even though the radiometric measurements were made over those watersh
eds that were burned in the same year. It was concluded that the burni
ng process might not completely remove a thatch layer of efficient mic
rowave absorption, which was developed through years of accumulation o
f senescent vegetation. Results from the analysis of these radiometric
data sets also suggest the need of an adequate estimation of vegetati
on biomass in order to obtain a reliable retrieval of surface soil moi
sture from L-band radiometric measurements. On the basis of the data a
cquired from the 1987 and 1989 field campaigns, the push broom microwa
ve radiometer (PBMR) measurements are likely to give errors of the ord
er of +/-0.065 g/cm(3) in surface soil moisture estimation if there ar
e no measurements of vegetation biomass. Measurements of vegetation bi
omass to an accuracy of +/-0.46 kg/m(2) improve the corresponding PBMR
estimation of surface soil moisture to an accuracy of +/-0.032 g/cm(3
).