The precipitation forecasts of four operational numerical weather predictio
n models over the Alpine region are evaluated and intercompared for two per
iods of interest to the Mesoscale Alpine Programme (MAP). The new analysis
of Alpine rainfall of Frei and Schar (1998) is used to validate the models.
It is found that the models have a tendency to overestimate the total prec
ipitation and the frequency of intense rain events over high orography. The
skill scores show good consistency between models, except for the ability
to forecast light rain or heavy rain events. The partition between convecti
ve and stratiform rainfall is rather variable between the models.