Answers are grounded in this paper and cite their sources.
Vertical profiles of aerosol concentration were measured on 8 occasions from McMurdo Station, Antarctica (78°S), between late August and early October 1992. Polar stratospheric clouds (PSCs) were observed on 6 of these soundings. The characteristics of PSCs, are ozone, were quite different above and below about 16 km. Above 16 km PSCs were variable in time, with particles >1.0 μm radius contributing significantly to the surface area, generally <8 μm 2 cm −3 . Below 16 km PSCs were much more stable and were dominated by high concentrations of smaller particles, <1.0 μm, with surface areas of 20–30 μm 2 cm −3 . This lower layer coincided with the altitude of the primary Pinatubo volcanic aerosol as measured in mid September and October, and with the 4 km region of the atmosphere where ozone was virtually completely destroyed over Antarctica in 1992.
No takes yet. Share an insight, caveat, or question.
Deshler et al. (1994) studied this question.
Synapse has enriched 10 related papers. Consider them for comparative context: