The present paper reports on extensive experiments performed on short, fixe
d, unheated conductor samples in an outdoor freezing rain simulator. Their
purpose is to relate the weight of ice (or, alternatively, the equivalent r
adial ice thickness) accreted on the samples with the associated weather co
nditions. Over 50 specimens have been obtained under environmental conditio
ns that encompass both wet and dry ice growths as well as several wind cond
itions. A nondimensionalization technique is devised to accommodate variati
ons in the imperfectly controlled test conditions. Consistent experimental
results could be discerned more clearly when the horizontal as well as the
vertical precipitation rate were measured. A strong linear correlation is f
ound between a dimensionless ice thickness and a dimensionless time. A simp
le model, Goodwin's model, is found to fit the experimental data surprising
ly well for both dry and wet ice growths.