% IMPORTANT: The following is UTF-8 encoded.  This means that in the presence
% of non-ASCII characters, it will not work with BibTeX 0.99 or older.
% Instead, you should use an up-to-date BibTeX implementation like “bibtex8” or
% “biber”.

@ARTICLE{Kalabokas:55629,
      author       = {Kalabokas, P. D. and Volz-Thomas, A. and Brioude, J. and
                      Thouret, V. and Cammas, J.-P. and Repapis, C. C.},
      title        = {{V}ertical ozone measurements in the troposphere over the
                      {E}astern {M}editerranean and comparison with {C}entral
                      {E}urope},
      journal      = {Atmospheric chemistry and physics},
      volume       = {7},
      issn         = {1680-7316},
      address      = {Katlenburg-Lindau},
      publisher    = {EGU},
      reportid     = {PreJuSER-55629},
      pages        = {3783 - 3790},
      year         = {2007},
      note         = {Record converted from VDB: 12.11.2012},
      abstract     = {Vertical ozone profiles measured in the period 1996-2002 in
                      the framework of the MOZAIC project (Measurement of Ozone
                      and Water Vapor by Airbus in Service Aircraft) for flights
                      connecting Central Europe to the Eastern Mediterranean basin
                      (Heraklion, Rhodes, Antalya) were analysed in order to
                      evaluate the high rural ozone levels recorded in the
                      Mediterranean area during summertime. The 77 flights during
                      summer (JJAS) showed substantially (10-12 ppb, $20-40\%)$
                      enhanced ozone mixing ratios in the lower troposphere over
                      the Eastern Mediterranean frequently exceeding the 60 ppb,
                      8-h EU air quality standard, whereas ozone between 700 hPa
                      and 400 hPa was only slightly (3-5 ppb, $5-10\%)$ higher
                      than over Central Europe. Analysis of composite weather maps
                      for the high and low ozone cases, as well as
                      back-trajectories and vertical profiles of carbon monoxide,
                      suggest that the main factor leading to high tropospheric
                      ozone values in the area is anticyclonic influence, in
                      combination with a persistent northerly flow in the lower
                      troposphere during summertime over the Aegean. On the other
                      hand the lowest ozone levels are associated with
                      low-pressure systems, especially the extension of the Middle
                      East low over the Eastern Mediterranean area.},
      keywords     = {J (WoSType)},
      cin          = {ICG-2},
      ddc          = {550},
      cid          = {I:(DE-Juel1)VDB791},
      pnm          = {Atmosphäre und Klima},
      pid          = {G:(DE-Juel1)FUEK406},
      shelfmark    = {Meteorology $\&$ Atmospheric Sciences},
      typ          = {PUB:(DE-HGF)16},
      UT           = {WOS:000248733100007},
      url          = {https://juser.fz-juelich.de/record/55629},
}