Estimate the rain volume reflectivity of a side-looking airborne SAR operating in the L band at 1.5 GHz for rain rates of 0.25 mm/hr, 1 mm/hr, 4 mm/hr, and 16 mm/Hr.
f = 1.5e9;
rr = [0.25 1 4 16];
Compute the rain volume reflectivity.
volref = rainreflectivity(f,rr);
Plot the rain volume reflectivity as a function of the rain rate.
Volume reflectivity (radar cross-section per unit volume) of rain in square meters
per cubic meter, returned as a matrix. The rows of volref
correspond to the radar frequency values in freq. The columns of
volref correspond to the rain rate values in
rr.
The rain clutter reflectivity is computed based on the commonly used
Marshall-Palmer drop-size distribution model. The model assumes raindrops are generally
small with respect to the wavelength and are nearly spherical, indicating Rayleigh
scattering.
The Marshall-Palmer model matches experimental results with measured data up to the
Ka-band. Additionally, rain is not a static target, and exhibits its own motion spectrum.
The motion spectrum is typically centered at some velocity with a recognizable velocity
bandwidth. Data suggests a velocity bandwidth sometimes as high as 8 m/s, with a median
velocity bandwidth of about 4 m/s.
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