Z–R power laws from disdrometer and TRMM-PR data are derived and compared.
Diversity of prefactor and exponent values of the estimated power laws is observed.
An overestimation of the rain rate by the TRMM-PR algorithm is found for stratiform rain.
Contemporary data from TRMM-PR and a polarimetric radar are analyzed and compared.
A great variability of rain rate in a TRMM-PR footprint is observed for convective rain.