rainreflectivity
Description
Examples
Rain Volume Reflectivity
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.
semilogx(rr,volref,'.-') xlabel('Rain Rate (mm/hr)') ylabel('Volume Reflectivity (dB/m)')
Input Arguments
freq
— Radar frequency
positive real scalar | vector
Radar frequency in hertz, specified as a positive real scalar or a vector.
Data Types: double
rr
— Rain rate
real scalar | vector
Rain rate in millimeters per hour, specified as a real scalar or a vector.
Data Types: double
pol
— Polarization of transmitted and received waves
'HH'
(default) | 'HV'
| 'VV'
| 'VH'
| 'RCPRCP'
| 'RCPLCP'
| 'LCPLCP'
| 'LR'
| 'HRCP'
| 'VLCP'
| 'RCPV'
| 'LCPH'
Polarization of transmitted and received waves, specified as one of these.
Value | Transmitted Wave | Received Wave |
---|---|---|
'HH' | Horizontal polarization | Horizontal polarization |
'HV' | Horizontal polarization | Vertical polarization |
'VV' | Vertical polarization | Vertical polarization |
'VH' | Vertical polarization | Horizontal polarization |
'RCPRCP' | Right-hand circular polarization | Right-hand circular polarization |
'RCPLCP' | Right-hand circular polarization | Left-hand circular polarization |
'LCPLCP' | Left-hand circular polarization | Left-hand circular polarization |
'LR' | Left-hand polarization | Right-hand polarization |
'HRCP' | Horizontal polarization | Right-hand circular polarization |
'VLCP' | Vertical polarization | Left-hand circular polarization |
'RCPV' | Right-hand circular polarization | Vertical polarization |
'LCPH' | Left-hand circular polarization | Horizontal polarization |
Data Types: char
| string
Output Arguments
More About
Marshall-Palmer Model
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.
Extended Capabilities
C/C++ Code Generation
Generate C and C++ code using MATLAB® Coder™.
Version History
Introduced in R2021a
See Also
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