Using parameterizations of cloud microphysics, a technique to forecast
supercooled cloud events is suggested. This technique can be coupled
on the mesoscale with a prognostic equation for cloud water to improve
aircraft icing forecasts. The procedure is validated using comparison
s with airborne measurements from the Canadian Atlantic Storms Program
. As an illustration of the application of this forecast technique, co
nstant-pressure maps showing regions of cloud ice, supercooled cloud w
ater, and cloud liquid water are presented for two particular cases.