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Application of Clutter Suppression Methods to a Geostationary Weather Radar Concept

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Figure

Table 1. Key NIS system parameters.
Figure 2. Doppler spectrum versus altitude. The strong, red area atlower center is the clutter return, extending to about 3 km altitude.
Figure 3. Reflectivity Z versus altitude. Blue solid thick line is theexpectation of the measured reflectivity, and blue dashed line includesfading noise.Red solid thick curve is the ‘truth’, i.e., expectationof the rain reflectivity, without surface clutter
Figure 4. Left, flow diagram of the algorithm. Right: illustrationdue to use of a staggered PRF (is narrowband near 0 m/s

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