The interpretation of the experimental evidence of the presence of a double
component in the distribution of rainfall annual maxima (RAM) observed alo
ng he Tyrrhenian coast of Italy is discussed here. Using a simple model for
rainfall storm generation the effect of the presence or absence of the Eur
opean blocking condition on the generation of the double component in the R
AM is investigated. The model is calibrated on the essential meteorological
characteristics of the Mediterranean storms provided both by remote sensin
g and high resolution raingauge data. It allows to give a physical explanat
ion for the variability of the parameters distribution with time observatio
n interval. The maxima extracted from the model generated rainfall time ser
ies show statistical properties very similar to those obtained by sample da
ta. In particular the model derived rainfall frequency curves and intensity
duration frequency curves show a good agreement with the observed ones. (C
) 2001 Elsevier Science Ltd. All rights reserved.