Radar backscattering data for surfaces of geological interest
Radar backscattering data for surfaces of geological interest
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Radar backscattering data for surfaces of geological interest
Laser optical radar measurement of atmospheric Raman backscattering by nitrogen, oxygen, and water vapor
Measuring wavelength dependence of backscatter from smooth randomly rough surface using acoustic waves in water
Extension of slope-facet model of radar backscatter from sea
Backscattered sun and skylight spectra from sea obtained from low flying aircraft as measure of chlorophyll concentration
Photochemical etching is most successful method for obtaining simulated microwave backscatter pattern from ocean surface. Process is adaptable to integrated circuit and thin film semiconductor fabrications. The attained horizontal resolution of 10 should improve with equipment refinement.
Report is described which considers the effect that the ocean's surface shape has on near-vertical backscatter. Report covers the statistical character of the surface, the relation between these statistics and electric field, the characteristics of the wave system, and electromagnetic scattering.
Spectral response measurements of man-made targets and surfaces for frequency variation analysis of electromagnetic backscatter
Estimation of total ozone from Nimbus 4 satellite measurements of backscattered ultraviolet earth radiance
Design, development, and characteristics of gamma backscatter atmosphere density sensor
Signal to noise ratios for coaxial laser radar system heterodyning signal backscattered from atmospheric aerosol
Linearly polarized lidar light scattering in spherically symmetrical uniformly distributed cloud water drops, investigating multiple backscattering effects on depolarization
Time dependent multiple backscattering of pulsed light for linearly polarized incident radiation
Ocean surface condition correlation to radar backscattering cross sections and wind velocity from scatterometer data
The Backscatter Ultraviolet (BUV) experiment aboard the Nimbus-4 satellite is discussed. This double monochromator experiment measures ultraviolet terrestrial radiance at 12 discrete wavelengths between 2550 A and 3400 A. Approximately 100 scans covering a 230 kilometer square are made between terminator crossings on the daylight side of the earth. A colinear photometer channel with the same field of view is used to derive the Lambert reflectivity of the lower boundary of the scattering atmosphere. The extraterrestrial solar irradiance is measured at the northern terminator. The instrument has currently produced almost three years of nearly continuous data which are being used to infer the high-level ozone distribution and total ozone on a global basis. The high-level ozone data have been verified by independent coincident rocket ozone soundings, and the total ozone values show good agreement with Dobson spectrophotometer determinations as well as those made with the Infrared Interferometer Spectrometer also on Nimbus-4.
The two-scale (small irregularities superimposed upon large undulations) scattering theory proposed by Semyonov was extended and used to compute microwave apparent temperature and the backscattering cross section from ocean surfaces. The effect of the small irregularities upon the scattering characteristics of the large undulations is included by modifying the Fresnel reflection coefficients; whereas the effect of the large undulations upon those of the small irregularities is taken into account by averaging over the surface normals of the large undulations. The same set of surface parameters is employed for a given wind speed to predict both the scattering and the emission characteristics at both polarizations.
A two-scale composite surface scattering theory was developed without using the noncoherent assumption. The surface is assumed electrically homogeneous and finitely conducting; the surface roughness may be nonuniform geometrically. The special forms of the terms for excluding the non-coherent assumption and the meanings of these terms are discussed. To gain insight into the mechanisms of backscattering, the results are compared with those obtained by previous theories. The comparison with NRL data shows satisfactory agreement for both horizontal and vertical polarization, especially for incident angles larger than 30 deg. For smaller incident angles, NASA/JSC data have been chosen for comparison and close agreement is again observed.
A confocal backscatter laser Doppler velocimeter (LDV) that measures two velocity components has been developed. This device requires only two incident beams polarized normally to one another. Moreover, the velocity components sensed are nearly orthogonal. The velocimeter employs a combined dual-scatter, local oscillator arrangement to obtain the bidirectional sensitivity. Two photodetectors are used, each sensing only one Doppler frequency proportional to one of the very nearly orthogonal velocity components. In addition, a single Bragg cell serves to frequency bias both velocity components in order to eliminate directional ambiguity. A differencing technique has also been incorporated to enhance the dual-scatter Doppler signal corresponding to the transverse velocity.