Using spectroscopic and electric measurements, vibrational and rotatio
nal molecular gas temperatures as well as free electron temperature an
d concentration were determined in different regions of a time-periodi
cal type, atmospheric pressure non-equilibrium low current gliding are
. It was shown that this discharge includes an initial quasi-equilibri
um zone, with the quasi-equilibrium temperature of 4 to 6 kK, and the
non-equilibrium zone with the electron temperature about 10 kK, the vi
brational temperature about 3 kK, rotational and translational tempera
tures from 1 to 1.5 kK. The transition between two mentioned zones coi
ncides with the phenomenon of the are ''length explosion'' already obs
erved in moderate-current gliding are.