Yj. Orsolini et al., LAYERING IN STRATOSPHERIC PROFILES OF LONG-LIVED TRACE SPECIES - BALLOON-BORNE OBSERVATIONS AND MODELING, J GEO RES-A, 103(D5), 1998, pp. 5815-5825
A series of balloon flights conducted in March 1993 from Aire-sur-Adou
r, in southern France, aimed at making in situ measurements of a varie
ty of trace gases in the polar vortex during a dynamically active peri
od. Meteorological analyses indicate that the balloons were launched w
hen the vortex edge was passing aloft. These mid latitude balloon flig
hts revealed coincident layering in long-lived tropospheric source gas
es such as nitrous oxide, methane and halocarbons as well. as in ozone
and water vapor. At low altitudes, well-resolved laminations appeared
clearly in all these gases. A layer of mid latitude air, enriched in
trace gases, was detected at the highest sampled level, near 15 mbar,
inducing a pronounced reversal in the profiles of tropospheric source
gases. Using global meteorological analyses, trace constituent data de
rived from the UARS observations and high-resolution advection models,
fine-scale distributions of ozone, nitrous oxide, methane, and haloca
rbons have been constructed. The calculations show qualitatively how s
uch profile reversal arises near 15 mbar, when a filament of air enric
hed in trace gases is drawn into the outer portion of the vortex. Very
high resolution calculations furthermore provide reasonable quantitat
ive agreement between predicted tracer mixing ratios and in situ ballo
on-borne measurements.