Articles | Volume 16, issue 20
https://doi.org/10.5194/acp-16-13341-2016
https://doi.org/10.5194/acp-16-13341-2016
Research article
 | 
28 Oct 2016
Research article |  | 28 Oct 2016

Analysis of the latitudinal variability of tropospheric ozone in the Arctic using the large number of aircraft and ozonesonde observations in early summer 2008

Gerard Ancellet, Nikos Daskalakis, Jean Christophe Raut, David Tarasick, Jonathan Hair, Boris Quennehen, François Ravetta, Hans Schlager, Andrew J. Weinheimer, Anne M. Thompson, Bryan Johnson, Jennie L. Thomas, and Katharine S. Law

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Cited articles

Abbatt, J. P. D., Thomas, J. L., Abrahamsson, K., Boxe, C., Granfors, A., Jones, A. E., King, M. D., Saiz-Lopez, A., Shepson, P. B., Sodeau, J., Toohey, D. W., Toubin, C., von Glasow, R., Wren, S. N., and Yang, X.: Halogen activation via interactions with environmental ice and snow in the polar lower troposphere and other regions, Atmos. Chem. Phys., 12, 6237–6271, https://doi.org/10.5194/acp-12-6237-2012, 2012.
AMAP: Assessment 2015: Black carbon and ozone as Arctic climate forcers. Arctic Monitoring and Assessment Programme (AMAP), Arctic Monitoring and Assessment Programme (AMAP), Oslo, Norway, 1–116, available at: http://www.amap.no/documents/doc/, 2015.
Ancellet, G.: CNRS ATR-42 aircraft ozone lidar observations, LATMOS/IPSL, UPMC Univ. Paris 06 Sorbonne Université, UVSQ, CNRS, Paris, France, available: ftp://polarcat@ftp.aero.jussieu.fr/Kanger/LidarO3/, 2009a.
Ancellet, G.: CNRS ATR-42 ozone in-situ measurements, LATMOS/IPSL, UPMC Univ. Paris 06 Sorbonne Universités, UVSQ, CNRS, Paris, France, avilable at: ftp://ftp.aero.jussieu.fr/Kanger/Data_ATR/, 2009b.
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An integrated analysis of all the ozone observations (lidar, sondes, and airborne in situ measurements) conducted during the 2008 IPY campaigns is performed and the processes that determine summer ozone concentrations over Greenland and Canada are discussed. Combined with a regional model simulation (WRFChem), the analysis of ozone, CO, and PV latitudinal and vertical variability allows the determination of the influence of stratospheric sources and biomass burning and anthropogenic emissions.
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