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Volume 16, issue 10
Atmos. Chem. Phys., 16, 6011–6025, 2016
https://doi.org/10.5194/acp-16-6011-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
Atmos. Chem. Phys., 16, 6011–6025, 2016
https://doi.org/10.5194/acp-16-6011-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.

Research article 18 May 2016

Research article | 18 May 2016

Airborne observation of mixing across the entrainment zone during PARADE 2011

Florian Berkes1,2,a, Peter Hoor1, Heiko Bozem1, Daniel Kunkel1, Michael Sprenger3, and Stephan Henne4 Florian Berkes et al.
  • 1Institute for Atmospheric Physics, Johannes Gutenberg University Mainz, Mainz, Germany
  • 2Department of Atmospheric Chemistry, Max Planck Institute for Chemistry, Mainz, Germany
  • 3Institute for Atmospheric and Climate Science, ETH Zurich, Zürich, Switzerland
  • 4Empa Swiss Federal Laboratories for Materials Science and Technology, Dübendorf, Switzerland
  • anow at: Institute of Energy and Climate Research-8: Troposphere, Forschungszentrum Jülich GmbH, Jülich, Germany

Abstract. This study presents the analysis of the structure and air mass characteristics of the lower atmosphere during the field campaign PARADE (PArticles and RAdicals: Diel observations of the impact of urban and biogenic Emissions) on Mount Kleiner Feldberg in southwestern Germany during late summer 2011. We analysed measurements of meteorological variables (temperature, moisture, pressure, wind speed and direction) from radio soundings and of chemical tracers (carbon dioxide, ozone) from aircraft measurements. We focus on the thermodynamic and dynamic properties that control the chemical distribution of atmospheric constituents in the boundary layer. We show that the evolution of tracer profiles of CO2 and O3 indicate mixing across the inversion layer (or entrainment zone). This finding is supported by the analysis of tracer–tracer correlations which are indicative for mixing and the relation of tracer profiles in relation to the evolution of the boundary layer height deduced from radio soundings. The study shows the relevance of entrainment processes for the lower troposphere in general and specifically that the tracer–tracer correlation method can be used to identify mixing and irreversible exchange processes across the inversion layer.

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We presented airborne measurements of CO2 and O3 across the entrainment zone over a semi-remote environment in southwestern Germany in late summer 2011 . For the first time CO2 and O3 were used as tracer to identify mixing through this transport barrier. We demonstrated that the tracer--tracer correlation of CO2 and O3 is a powerful tool to identify entrainment and mixing.
We presented airborne measurements of CO2 and O3 across the entrainment zone over a semi-remote...
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