Brightband effects are one of the more important causes of vertical va
riability of reflectivity and severely affect the accuracy of rainfall
estimates from ground-based radar. Monte Carlo simulation experiments
are performed to investigate the efficiency of a procedure for the co
rrection of errors related to the vertical variability of reflectivity
. The simulation model generates three-dimensional radar reflectivity
fields. Brightband effects are simulated through a physically based mo
del of melting-layer reflectivity observations. Sensitivity of the cor
rection procedure for a number of different precipitation scenarios an
d radar systems is analyzed. Overall, the identification method is fou
nd to be a robust procedure for correction of brightband effects. Resu
lts indicate a dependence of the effectiveness of the correction proce
dure on mean altitude and spatial variability of the melting layer.