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@ARTICLE{Auvray:57798,
      author       = {Auvray, M. and Bey, I. and Llull, E. and Schultz, M. G. and
                      Rast, S.},
      title        = {{A} model investigation of the impact of long-range
                      transport on tropospheric ozone chemical tendencies},
      journal      = {Journal of Geophysical Research},
      volume       = {112},
      issn         = {0148-0227},
      address      = {Washington, DC},
      publisher    = {Union},
      reportid     = {PreJuSER-57798},
      pages        = {D05304},
      year         = {2007},
      note         = {Record converted from VDB: 12.11.2012},
      abstract     = {The impact of continental outflow on the ozone chemical
                      tendencies (i.e., production and loss rates) is quantified
                      in the North Atlantic and northwest Pacific regions using
                      the GEOS-Chem and the MOZECH global models of chemistry and
                      transport. The ozone tendencies simulated by these global
                      models are compared to box model simulations constrained by
                      observations in different regions and seasons. The two
                      global models generally capture the seasonal and regional
                      variations of the ozone tendencies. The largest
                      discrepancies between the ozone tendencies from the box
                      model and those from the global models are found in the
                      lower troposphere of the eastern North Atlantic during the
                      ACSOE campaign and are attributed to differences between
                      chemical schemes and too strong NOx concentrations in the
                      global models. The background and plume (i.e., impacted by
                      continental outflow) environments are differentiated over
                      the oceanic areas using criteria based on simulated daily
                      mean CO concentrations. The ozone tendencies in the plume
                      environment differ from that in the background over the
                      entire column in North Atlantic and northwest Pacific at all
                      seasons. According to the models, net ozone production is
                      enhanced by 2 to 6 ppbv/day in the boundary layer and by 1
                      to 3 ppbv/ day in the upper troposphere, whereas the effect
                      of pollution ranges from -1 ppbv/day to +1 ppbv/day in the
                      middle troposphere (3-7 km), depending on the model used.
                      The different responses of the two models are determined by
                      differences in the water vapor distributions relative to
                      those of pollutants in the plumes. In particular, GEOS-Chem
                      tends to transport pollution in a drier sector of cyclones
                      than MOZECH.},
      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:000244899100002},
      doi          = {10.1029/2006JD007137},
      url          = {https://juser.fz-juelich.de/record/57798},
}