To iIlvestigate the possibility to use passive microwave brightness tempera
ture measurements to distinguish stratiform and convective regions of mesos
cale convective systems (MCSs) over land background, a new polarized radiat
ive transfer Monte Carlo code has been developed. The code is based on a fo
rward scheme and is used to investigate the relation between the brightness
temperature differences for the horizontal and vertical polarization (Delt
aT(v-H)) observed in the stratiform region of these cloud systems and the c
loud microphysics. Radiative transfer computations have been performed on a
microphysical-dynamical cloud model and the results are presented together
with the algorithm description. (C) 2001 International Astronautical Feder
ation. Published by Elsevier Science Ltd. All rights reserved.