A laboratory experiment is performed in a cold chamber to produce micr
odischarges between frozen hydrometeors. A charged icicle is placed cl
ose to an uncharged one connected to a transient analyser. The electri
c current signature obtained during each event is then studied and cha
racterized in function of both temperature and net charge. The existen
ce of a transition temperature of about -15 degrees C is detected, whe
reas net charge clearly governs the microdischarge characteristics. Fu
rthermore, the radiated electric field is calculated and the spectral
analysis, by means of fast Fourier transform, shows that this elementa
ry phenomenon radiates within the VHF range. Comparisons are made with
previous similar work by Chauzy and Kably (1989) on microdischarges b
etween water drops.