IEEE International Conference on Radar
DOI: 10.1109/radar.1990.201162
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Modeling the spectral structure of ducted sea clutter

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“…The backscattered signal in a Radar anemometer originates from radiation scattered by turbulent eddies embodied in the mean wind field. The received power from a distribution of scatterers in the range cell is27, PTALtR = 4irR2 (9) where P-i-is the transmitted power, A is the effective aperture area, R is the range to the scattering volume, r is the reflectivity, and iR is the range resolution. However, the reflectivity of clear-air turbulent eddies is much lower than for precipitating hydrometeors ( Table 2), and is given by, c1ear-air = O38Cr2 (10) where C2nr is the atmospheric structure factor which is a function of the pressure, temperature, and moisture content of the atmosphere.…”
Section: Piezoresistive Materialsmentioning
confidence: 99%
“…The backscattered signal in a Radar anemometer originates from radiation scattered by turbulent eddies embodied in the mean wind field. The received power from a distribution of scatterers in the range cell is27, PTALtR = 4irR2 (9) where P-i-is the transmitted power, A is the effective aperture area, R is the range to the scattering volume, r is the reflectivity, and iR is the range resolution. However, the reflectivity of clear-air turbulent eddies is much lower than for precipitating hydrometeors ( Table 2), and is given by, c1ear-air = O38Cr2 (10) where C2nr is the atmospheric structure factor which is a function of the pressure, temperature, and moisture content of the atmosphere.…”
Section: Piezoresistive Materialsmentioning
confidence: 99%