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Battaglia, A., C. Simmer, and H. Czekala (2006), Three-dimensional effects in polarization signatures as observed from precipitating clouds by low frequency ground-based microwave radiometers, Atmos. Chem. Phys., 6, 4383–4394, doi:10.5194/acp-6-4383-2006.
Czekala, H. (1998), Effects of ice particle shape and orientation on polarized microwave radiation for off-nadir problems, Geophys. Res. Lett., 25(10), 1669–1672.
Defer, E., V. S. Galligani, C. Prigent, and C. Jimenez (2014), First observations of polarized scattering over ice clouds at close-to-millimeter wavelengths (157 GHz) with MADRAS on board the Megha-Tropiques mission, J. Geophys. Res., 119(21), 12301–12316, doi:10.1002/2014JD022353.
Deiveegan, M., C. Balaji, and S. P. Venkateshan (2008), A polarized microwave radiative transfer model for passive remote sensing, Atmos. Res., 88, 277–293, doi:10.1016/j.atmosres.2007.11.023.
Evans, K. F. and G. L. Stephens (2010), Many polarized radiative transfer models, J. Quant. Spectrosc. Radiat. Transfer, 111, 1686–1688, doi:10.1016/j.jqsrt.2010.01.029.
Landi Degl'Innocenti, E. and M. Landi Degl'Innocenti (1985), On the solution of the radiative transfer equations for polarized radiation, Sol. Phys., 97, 239–250.
Okamoto, H., K. Sato, and Y. Hagihara (2010), Global analysis of ice microphysics from CloudSat and CALIPSO: Incorporation of specular reflection in lidar signals, J. Geophys. Res., 115, D22209, doi:10.1029/2009JD013383.
Prigent, C., J. R. Pardo, M. I. Mishchenko, and W. B. Rossow (2001), Microwave polarized signatures generated within cloud systems: Special Sensor Microwave Imager (SSM/I) observations interpreted with radiative transfer simulations, J. Geophys. Res., 106(D22), 28243–28258.
Prigent, C., E. Defer, J. R. Pardo, C. Pearl, W. B. Rossow, and J.-P. Pinty (2005), Relations of polarized scattering signatures observed by the TRMM Microwave Instrument with electrical processes in cloud systems, Geophys. Res. Lett., 32, L04810, doi:10.1029/2004GL022225.
Xie, X. and J. Miao (2011), Polarization difference due to nonrandomly oriented ice particles at millimeter/submillimeter waveband, J. Quant. Spectrosc. Radiat. Transfer, 112, 1090–1098, doi:10.1016/j.jqsrt.2010.11.020.