We made a comparison between man-made 24-h thunderstorm forecasts (subjecti
ve forecasts) and 24-h pure index thunderstorm forecasts (objective forecas
ts). The forecasts concern the plane of Friuli-Venezia Giulia region (NE It
aly) during summer. Subjective forecasts are based on forecaster interpreta
tion of numerical models outputs and forecaster's experience, while objecti
ve forecasts use models outputs and the thunderstorm climatology of our reg
ion to issue two independent indexes. Both these indexes are calculated by
a linear combination of meteorological variables extracted from the Europea
n Centre for Medium Range Forecast (ECMWF) model. In one case, the coeffici
ents of the combination were obtained by a linear multiregression over 8 ye
ars of data, while in the other, the biserial correlation coefficient was m
aximized on a subset of 2 years. To estimate the quality of forecasts, we u
sed the data collected during the summer of 1998 and 1999; thunderstorm day
s are defined by lightning data and ground stations observations. The joint
probability density functions of forecasts and observations have been used
to study the forecast quality. We also studied the reliability diagrams of
subjective forecasts. We found that subjective forecast skill and objectiv
e forecast skill are comparable although there were some differences as wel
l. Subjective forecasts have a low false alarm rate (FAR) and they showed g
ood facility in forecasting days without thunderstorms, but they score low
in probability of detection (POD). Objective forecasts, in contrast, showed
lower FAR and facility in forecasting stormy days but detected thunderstor
ms better than subjective forecasts. There are significant fluctuations in
forecasts' performance from 1998 to 1999 summer seasons. This is likely due
to variation in thunderstorm climatology and thunderstorm type frequencies
. Furthermore, feedback of past performances could have played an important
role in subjective forecasts. (C) 2001 Elsevier Science B.V. All rights re
served.