Aerosols as dynamical tracers in the lower stratosphere: Ozone versus aerosol correlation after the Mount Pinatubo eruption

Journal Article · Tue Jun 20 04:00:00 EDT 1995 · Journal of Geophysical Research

DOI:https://doi.org/10.1029/95JD00016· OSTI ID:136164

Borrmann, S ^[1]; Dye, J E; Baumgardner, D ^[2]

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1. Johannes Gutenberg Universitaet, Mainz (Germany)
2. National Center for Atmospheric Research, Boulder, CO (United States); and others

Stratospheric in situ aerosol and ozone measurement aboard the NASA-operated ER-2 high-altitude research aircraft from August 1991 to May 1993 provide an opportunity to document the temporal evolution of the correlation between the stratospheric aerosol and the ozone from shortly after the Mount Pinatubo eruption until almost two years later. The observations show that at midlatitudes a linear relationship evolves between aerosol surface (or number) mixing ratios and ozone at altitudes ranging from slightly above the tropopause to 14-16 km. This correlation is linear for values of ozone from 200 to 1300 parts per billion by volume and for potential temperatures between 310 K and 467 K. The linear correlation persisted from late December 1991 until early March 1992 but degraded by October 1992. 32 refs., 17 figs., 2 tabs.

• OSTI ID: 136164
• Journal Information: Journal of Geophysical Research, Journal Name: Journal of Geophysical Research Journal Issue: D6 Vol. 100; ISSN JGREA2; ISSN 0148-0227
• Country of Publication: United States
• Language: English

Related Subjects

54 ENVIRONMENTAL SCIENCES
AEROSOLS
CORRELATIONS
ECOLOGICAL CONCENTRATION
OZONE
STRATOSPHERE
TRACER TECHNIQUES
VOLCANIC GASES