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@ARTICLE{Berkes:276603,
      author       = {Berkes, Florian and Hoor, P. and Bozem, H. and Kunkel, D.
                      and Sprenger, M. and Henne, S.},
      title        = {{A}irborne observation of mixing across the entrainment
                      zone during {PARADE} 2011},
      journal      = {Atmospheric chemistry and physics / Discussions},
      volume       = {15},
      number       = {20},
      issn         = {1680-7375},
      address      = {Katlenburg-Lindau},
      publisher    = {EGU},
      reportid     = {FZJ-2015-06957},
      pages        = {29171 - 29212},
      year         = {2015},
      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.},
      cin          = {IEK-8},
      ddc          = {550},
      cid          = {I:(DE-Juel1)IEK-8-20101013},
      pnm          = {243 - Tropospheric trace substances and their
                      transformation processes (POF3-243)},
      pid          = {G:(DE-HGF)POF3-243},
      typ          = {PUB:(DE-HGF)16},
      doi          = {10.5194/acpd-15-29171-2015},
      url          = {https://juser.fz-juelich.de/record/276603},
}