BALLOON OBSERVATIONS OF STRATOSPHERIC ELECTRICITY ABOVE THE SOUTH-POLE - VERTICAL ELECTRIC-FIELD, CONDUCTIVITY, AND CONDUCTION CURRENT

This paper summarizes the results of measurements of the electrical conductivity-sigma and vertical component of the vector electric field E(z) acquired from eight stratosphcric balloon flights launched from Amundsen-Scott Station, South Pole, in the austral summer of 1985 1986. The major findings of this research are as follows: (1) The data contribute to the set of global atmospheric electricity measurements and extend the work of COBB [(1977), Atmospheric electric measurements at the South Pole. In Electrical Processes in Atmospheres, DOLEZALEK H. and REITER R. (eds), pp. 161-167. Steinkopf, Darmstadt, F.R.G.] to determine the electrical environment of the south polar region. (2) The average vertical profile of the conductivity at the South Pole, when compared with profiles obtained at other Antarctic locations, suggests that the conductivity scale height may increase with increasing geomagnetic latitude across the polar cap. (3) The conductivity profiles measured at the South Pole and other Antarctic locations differ significantly from polar cap model profiles. On the basis of these measurements, the model profiles appear to require modification. (4) The magnitudes of the E(z) profiles were observed to vary from day-to-day by a factor of > 2. (5) In all of the flights the air-Earth conduction current J(z), calculated as the product of E(z) and sigma, decreased with altitude in agreement with previous direct measurements of the air-Earth current by COBB [(1977), Atmospheric electric measurements at the South Pole. In Electrical Processes in Atmospheres, DOLEZALEK H. and REITER R. (eds), pp. 161-167. Steinkopf, Darmstadt, F.R.G.]. (6) The magnitude of J, was 2-3 times larger than the global average, which can be attributed to the lower columnar resistance of the atmosphere above the high-elevation Antarctic plateau. The magnitude of J(z) agrees with that observed by Cobb, if the Cobb measurements are multiplied by the FEW and WEINHEIMER [(1986), Factor of 2 error in balloon-borne atmospheric conduction current measurements. J. geophys. Res. 91, 10937] correction factor of 2. (7) E(z), from all of the flights during times of balloon float demonstrates characteristics of the classical 'Carnegie' diurnal variation, which is indicative of global influences on the ionospheric potential. (8) The influence of geomagnetic activity was observed as a decrease in the amplitude of the diurnal variation of E(z) with increasing geomagnetic activity index K(p), which is the predicted effect at the South Pole of the magnetospheric polar-cap potential superimposed on the 'Carnegie' potential variation.