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GEOPHYSICAL RESEARCH LETTERS,
VOL. 20, NO. 12,
PAGES 1187–1190,
1993
ON THE RELATIONSHIP BETWEEN STRATOSPHERIC AEROSOLS AND NITROGEN DIOXIDE
M. J. Mills
A. O. Langford
T. J. O'Leary
K. Arpag
H. L. Miller
M. H. Proffitt
R. W. Sanders
S. Solomon
Abstract
Observations of the stratospheric NO2 column amount over the Colorado mountains during January, February, and March, 1992 are compared to concurrent lidar measurements.
During this period, large aerosol amounts due to the volcanic material injected into the stratosphere by Mt. Pinatubo were
observed over Colorado. The observed NO2 column displays a strong anti-correlation with increasing amounts of stratospheric aerosol near 25–30 km for relatively low
aerosol loadings. At higher aerosol loadings, the NO2 response appears to saturate, displaying little further reduction. The reasons for the altitude dependence of this relationship
are probed with a one-dimensional stratospheric model, and it is shown that such a saturation response is to be expected for
conditions where the heterogeneous reaction between N2O5 and H2O dominates the NOx chemistry, as in Prather [1992]. The results therefore provide evidence that heterogeneous reactions influence the chemical
composition of the mid-latitude stratosphere, and in the general manner predicted by theory.
Received 1
November
1992;
accepted 19
April
1993.
Subscriber Access to Full Article (Nonsubscribers may purchase for $9.00, Includes print PDF)
Citation: Mills, M. J., A. O. Langford, T. J. O'Leary, K. Arpag, H. L. Miller, M. H. Proffitt, R. W. Sanders, and S. Solomon
(1993),
ON THE RELATIONSHIP BETWEEN STRATOSPHERIC AEROSOLS AND NITROGEN DIOXIDE,
Geophys. Res. Lett.,
20(12),
1187–1190.
Copyright 1993 by the American Geophysical Union.
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