论文信息 - Satellite microwave observations of the Utah Great Salt Lake Desert

Satellite microwave observations of the Utah Great Salt Lake Desert

Microwave data acquired over the Great Salt Lake Desert area by sensors aboard Skylab and Nimbus 5 indicate that the microwave emission and backscatter were strongly influenced by contributions from subsurface layers of sediment saturated with brine. This phenomenon was observedby Skylab's S-194 radiometer operating at 1.4 GHz, S-193 RADSCAT (Radiometer-Scatterometer) operating at 13.9 GHz, and the Nimbus 5 ESMR (Electrically Scanning Microwave Radiometer) operating at 19.35 GHz. The availability of ESMR data over an 18-month period allowed an investigation of temporal variations.

[1] M. Busby. Annual runoff in the conterminous United States , 1966 .

[2] A. Stogryn,et al. Equations for Calculating the Dielectric Constant of Saline Water (Correspondence) , 1971 .

[3] T. Schmugge,et al. Remote sensing of soil moisture with microwave radiometers , 1974 .

[4] Allan J. Delaney,et al. Dielectric properties of soils at UHF and microwave frequencies 36R. J. Geophys. Res. V79, N11, Apr. 1974, P1699–1708 , 1974 .

[5] R. Moore,et al. Soil moisture detection by Skylab's microwave sensors. [radiometer/scatterometer measurements of Texas , 1974 .

[6] G. Kenney. Skylab program. Earth resources experiment package. Sensor performance report. Volume 7 (S190B): SL2, SL3 and SL4 evaluations , 1974 .

[7] F. Ulaby. Radar measurement of soil moisture content , 1974 .

[8] Richard K. Moore,et al. Active microwave measurement of soil water content , 1974 .

[9] F. T. Ulaby,et al. REMOTE SENSING OF SOIL MOISTURE BY SKYLAB RADIOMETER AND SCATTEROMETER SENSORS. , 1975 .