“…Using inverse modelling, the imaginary part can be calculated and calibrated with soil salinity (Bell et al, 2001;Taylor et al, 1996;Yun et al, 2003). Soil salinity classes have been successfully derived on a local scale (b500 km 2 ) with the C-, P-, and L-bands of airborne and spaceborne radar systems; best results are obtained using L-band data because long wavelengths penetrate soil and vegetation to a greater extent than higher frequencies (Bell et al, 2001;Lasne et al, 2008;Taylor et al, 1996).…”