Nitric acid in cirrus clouds

Uptake of nitric acid (HNO 3 ) in Arctic cirrus ice crystals was observed on 11 February 2003 by in-situ instruments onboard the M55 Geophysica aircraft. The cirrus cloud with a mean ice water content of 5.4 mg m -3 covered northern Scandinavia for several hours and extended up to the thermal tropop...

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Bibliographic Details
Published in:Geophysical Research Letters
Main Authors: Voigt, C., Schlager, H., Ziereis, H., Kärcher, B., Luo, B.P., Schiller, C., Krämer, M., Popp, P.J., Irie, H., Kondo, Y.
Format: Article in Journal/Newspaper
Language:unknown
Published: Wiley 2006
Subjects:
Atmosphärische Spurenstoffe
Arctic
Online Access:https://elib.dlr.de/22631/
Description
Summary:Uptake of nitric acid (HNO 3 ) in Arctic cirrus ice crystals was observed on 11 February 2003 by in-situ instruments onboard the M55 Geophysica aircraft. The cirrus cloud with a mean ice water content of 5.4 mg m -3 covered northern Scandinavia for several hours and extended up to the thermal tropopause at 12.3 km. Within the cirrus region, on average 9% of the total HNO 3 measured as reactive nitrogen (NOy) is present in ice particles, increasing to 19% at temperatures below 205 K. In contrast to previous studies, we discuss the HNO 3 uptake in ice in terms of HNO 3 /H 2 O molar ratios in ice crystals. The HNO 3 content of the ice increases with increasing gas phase HNO 3 concentrations and decreasing temperatures. Enhanced uptake of HNO 3 in ice and heterogeneous chemistry on cold cirrus clouds may disturb the upper tropospheric ozone budget.

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