Method of extracting phase errors caused by the atmosphere in the backscatter signal of a coherent imaging radar system carried by a carrier from radar raw data and apparatus for carrying out the method
First Claim
1. A method of extracting phase errors caused by the atmosphere in the backscatter signal of a coherent imaging radar system carried by a carrier from radar raw data in whichfor imaging areas with different backscatter ratios over a predetermined period of time successive azimuth spectra are continuously formed anda frequency offset (Δ
- F(t)) of the backscatter ratio component is obtained by determining the position of the maximum of the correlations between two respective immediately successively formed azimuth spectra,wherein;
performing a double integration of the difference of the frequency offset (Δ
F(t)) and a desired value (Δ
Fsoll) of the frequency offset, the frequency offset desired value (Δ
Fsoll) being determined either from the carrier forward velocity (Vv) or by a low-pass filtering of the frequency offset (Δ
F(t)), andstandardizing a result of the double integration by multiplying said result with a constant of (2π
/Δ
t) to obtain the phase error (φ
e (t)).
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Abstract
In a method of extracting phase errors caused by the atmosphere in the backscatter signal of an on-board coherent imaging radar system from radar raw data, firstly to image areas with different backscatter ratios over a predetermined period of time consecutive azimuth spectra are continuously formed. Thereupon, a frequency offset (ΔF(t)) of the backscatter ratio component is obtained by determining the location of the maximum of the correlations between two respective immediately consecutively formed azimuth spectra. Then, a double integration for the difference of the frequency offset (ΔF(t)) and a desired value (ΔFsoll) of the frequency offset is carried out, the frequency offset desired value (ΔFsoll) being determined either from the carrier forward velocity (Vv) or by a low-pass filtering of the frequency offset (ΔF(t)), and finally for standardization the result of the double integration is multiplied by a constant (2π/Δt) to obtain thereby the phase error (φe (t)).
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Citations
2 Claims
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1. A method of extracting phase errors caused by the atmosphere in the backscatter signal of a coherent imaging radar system carried by a carrier from radar raw data in which
for imaging areas with different backscatter ratios over a predetermined period of time successive azimuth spectra are continuously formed and a frequency offset (Δ - F(t)) of the backscatter ratio component is obtained by determining the position of the maximum of the correlations between two respective immediately successively formed azimuth spectra,
wherein; performing a double integration of the difference of the frequency offset (Δ
F(t)) and a desired value (Δ
Fsoll) of the frequency offset, the frequency offset desired value (Δ
Fsoll) being determined either from the carrier forward velocity (Vv) or by a low-pass filtering of the frequency offset (Δ
F(t)), andstandardizing a result of the double integration by multiplying said result with a constant of (2π
/Δ
t) to obtain the phase error (φ
e (t)).
- F(t)) of the backscatter ratio component is obtained by determining the position of the maximum of the correlations between two respective immediately successively formed azimuth spectra,
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2. An apparatus for extracting phase errors caused by the atmosphere in the backscatter signal of a coherent imaging radar system carried by a carrier from radar raw data comprising:
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means for detecting an azimuth spectrum to form continuously successive azimuth spectra, means for correlation formation between two respective directly successively formed azimuth spectra and means for forming the maximum of the correlation and determining the frequency offset (Δ
F(t));means for forming a difference from the frequency offset (Δ
F(t)) and a desired value (Δ
Fsoll) of the frequency offset, the desired frequency offset (Δ
Fsoll) being determinable from the carrier forward velocity (Vv) or by a filtering of the frequency offset (Δ
F(t)) by means of a low-pass filter;two integrating units connected in series and following said difference-forming means; and a standardizing unit which follows the second integrating unit and at the output of which the phase error (φ
e (t)) caused by the atmosphere is obtained.
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Specification