In many cold climate countries, it is becoming increasingly important
to monitor transmission line icing. Indeed, by knowing in advance of l
ocalized danger for icing overloads, electric utilities can take measu
res in time to prevent generalized failure of the power transmission n
etwork. Recently in Canada, a study was made to compare the estimation
of a few icing models working from meteorological data in estimating
ice loads for freezing rain events. The models tested were using only
standard meteorological parameters, i.e. wind speed and direction, tem
perature and precipitation rate. This study has shown that standard me
teorological parameters can only achieve very limited accuracy, especi
ally for longer icing events. However, with the help of an additional
instrument monitoring the icing rate intensity, a significant improvem
ent in model prediction might be achieved. The icing rate meter (IRM)
which counts icing and de-icing cycles per unit time on a standard pro
be can be used to estimate the icing intensity. A cable icing estimati
on is then made by taking into consideration the accretion size, tempe
rature, wind speed and direction, and precipitation rate. In this pape
r, a comparison is made between the predictions of two previously test
ed models (one obtained and the other reconstructed from their descrip
tion in the public literature) and of a model based on the icing rate
meter readings. The models are tested against nineteen events recorded
on an icing test line at Mt. Valin, Canada, during the winter season
1991-92. These events are mostly rime resulting from in-cloud icing. H
owever, freezing rain and wet snow events were also recorded. Results
indicate that a significant improvement in the estimation is attained
by using the icing rate meter data together with the other standard me
teorological parameters.