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Observations of high concentrations of total reactive nitrogen (NO y ) and nitric acid (HNO 3 ) in the lower Arctic stratosphere during the Stratosphere‐Troposphere Experiment by Aircraft Measurements (STREAM) II campaign in February 1995

1997; American Geophysical Union; Volume: 102; Issue: D19 Linguagem: Inglês

10.1029/97jd02012

2156-2202

H. Fischer, A. Waibel, M. Welling, F. G. Wienhold, T. Zenker, Paul J. Crutzen, Frances H. Arnold, V. Bürger, Johannes Schneider, Ahron Bregman, Jos Lelieveld, P. Siegmund,

Atmospheric and Environmental Gas Dynamics

Simultaneous in situ measurements of NO y , HNO 3 , O 3 , N 2 O, and CO have been performed in the lower stratosphere during the Stratosphere‐Troposphere Experiment by Aircraft Measurements (STREAM) II intensive winter campaign in February 1995 from Kiruna airport (northern Sweden) with a Cessna Citation II twinjet aircraft up to a maximum altitude of 12.8 km. The flights were coordinated with the Arctic Second European Stratospheric Arctic and Midlatitude Experiment (SESAME) winter campaign. Strongly elevated levels of total reactive nitrogen (NO y ) and its most abundant contributing species, nitric acid (HNO 3 ), with mixing ratios up to 9 parts per billion by volume (ppbv), were observed during all flights at altitudes near 12 km. On average, the measured NO y concentrations exceed the expected levels by a factor of 2–3. Normal background NO y has been calculated from observed N 2 O mixing ratios using the NO y ‐N 2 O correlation reported for the undisturbed northern hemisphere. This indicates that subsidence of air in the vortex alone cannot explain these findings. We propose that the elevated NO y concentrations were caused by nitrification of the lower stratosphere associated with sedimentation and evaporation of polar stratospheric cloud particles that carry down HNO 3 from higher altitudes, that is, from altitudes up to about 25 km.