Observations of high concentrations of total reactive nitrogen (NOy) and nitric acid (HNO3) in the lower Arctic stratosphere during the stratosphere-troposphere experiment by aircraft measurements (STREAM) II campaign in February 1995

被引:33
作者
Fischer, H
Waibel, AE
Welling, M
Wienhold, FG
Zenker, T
Crutzen, PJ
Arnold, F
Burger, V
Schneider, J
Bregman, A
Lelieveld, J
Siegmund, PC
机构
[1] MAX PLANCK INST NUCL PHYS, D-69117 HEIDELBERG, GERMANY
[2] UNIV UTRECHT, INST MARINE & ATMOSPHER RES, NL-3584 CC UTRECHT, NETHERLANDS
[3] ROYAL NETHERLANDS METEOROL INST, KNMI, NL-3730 AE DE BILT, NETHERLANDS
关键词
D O I
10.1029/97JD02012
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
Simultaneous in situ measurements of NOy, HNO3, O-3, N2O, 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 (NOy) and its most abundant contributing species, nitric acid (HNO3), 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 concentrations exceed the expected levels by a factor of 2-3. Normal background NOy has been calculated from observed N2O mixing ratios using the NOy-N2O 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 NOy concentrations were caused by nitrification of the lower stratosphere associated with sedimentation and evaporation of polar stratospheric cloud particles that carry down HNO3 from higher altitudes, that is, from altitudes up to about 25 km.
引用
收藏
页码:23559 / 23571
页数:13
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