Atmospheric Chemistry and Physics Discussions www.atmos-chem-phys-discuss.net 1680-7367 1680-7375 9 3 2009 10.5194/acpd-9-14165-2009 http://www.atmos-chem-phys-discuss.net/9/14165/2009/ http://www.atmos-chem-phys-discuss.net/9/14165/2009/acpd-9-14165-2009.html http://www.atmos-chem-phys-discuss.net/9/14165/2009/acpd-9-14165-2009.pdf 14165 14187 2009-06-30 Airborne measurements of the nitric acid partitioning in persistent contrails D. Schäuble dominik.schaeuble@dlr.de C. Voigt B. Kärcher P. Stock H. Schlager M. Krämer C. Schiller R. Bauer N. Spelten M. de Reus M. Szakáll S. Borrmann U. Weers Th. Peter Deutsches Zentrum für Luft- und Raumfahrt, Institut für Physik der Atmosphäre, Oberpfaffenhofen, Germany Institut für Physik der Atmosphäre, Johannes-Gutenberg Universität Mainz, Mainz, Germany Institut für Stratosphärenforschung, FZ Jülich, Jülich, Germany Max-Planck-Institut für Chemie, Mainz, Germany Institut für Atmosphäre und Klima, ETH Zürich, Zürich, Switzerland This study reports the first systematic measurements of nitric acid (HNO₃) uptake in contrail ice particles at typical aircraft cruise altitudes. During the CIRRUS-III campaign cirrus clouds and almost 40 persistent contrails were probed with in situ instruments over Germany and Northern Europe in November 2006. Besides reactive nitrogen, water vapor, cloud ice water content, ice particle size distributions, and condensation nuclei were measured during 6 flights. Contrails with ages up to 8 hours were detected at altitudes 10–11.5 km and temperatures 211–220 K. These contrails had a larger ice phase fraction of total nitric acid (HNO₃^ice/HNO₃^tot = 6%) than the ambient cirrus layers (3%). On average, the contrails contained twice as much HNO₃^ice as the cirrus clouds, 14 pmol/mol and 6 pmol/mol, respectively. Young contrails with ages below 1 h had a mean HNO₃^ice of 21 pmol/mol. The contrails had higher nitric acid to water molar ratios in ice and slightly higher ice water contents than the cirrus clouds under similar meteorological conditions. The differences in ice phase fractions and molar ratios between developing contrails and cirrus are likely caused by high plume concentrations of HNO₃ prior to contrail formation. The location of the measurements in the top region of frontal cirrus layers might account for slight differences in the ice water content between contrails and adjacent cirrus clouds. 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