% 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{Gressent:172736,
      author       = {Gressent, Alicia and Sauvage, Bastien and Defer, Eric and
                      Pätz, Hans-Werner and Thomas, Karin and Holle, Ronald and
                      Cammas, Jean-Pierre and Nédélec, Philippe and Boulanger,
                      Damien and Thouret, Valérie and Volz-Thomas, Andreas},
      title        = {{L}ightning {NO}x influence on large-scale {NO}y and {O}3
                      plumes observed over the northern mid-latitudes},
      journal      = {Tellus / B},
      volume       = {66},
      issn         = {1600-0889},
      address      = {Stockholm},
      publisher    = {Inst.},
      reportid     = {FZJ-2014-06180},
      pages        = {25544},
      year         = {2014},
      abstract     = {This paper describes the NOy plumes originating from
                      lightning emissions based on 4 yr (2001–2005) of MOZAIC
                      measurements in the upper troposphere of the northern
                      mid-latitudes, together with ground- and space-based
                      observations of lightning flashes and clouds. This analysis
                      is primarily for the North Atlantic region where the MOZAIC
                      flights are the most frequent and for which the measurements
                      are well representative in space and time. The study
                      investigates the influence of lightning NOx (LNOx) emissions
                      on large-scale (300–2000 km) plumes (LSPs) of NOy. One
                      hundred and twenty seven LSPs $(6\%$ of the total MOZAIC NOy
                      dataset) have been attributed to LNOx emissions. Most of
                      these LSPs were recorded over North America and the Atlantic
                      mainly in spring and summer during the maximum lightning
                      activity occurrence. The majority of the LSPs $(74\%)$ is
                      related to warm conveyor belts and extra-tropical cyclones
                      originating from North America and entering the
                      intercontinental transport pathway between North America and
                      Europe, leading to a negative (positive) west to east NOy
                      (O3) zonal gradient with −0.4 (+18) ppbv difference during
                      spring and −0.6 (+14) ppbv difference in summer. The NOy
                      zonal gradient can correspond to the mixing of the plume
                      with the background air. On the other hand, the O3 gradient
                      is associated with both mixing of background air and with
                      photochemical production during transport. Such
                      transatlantic LSPs may have a potential impact on the
                      European pollution. The remaining sampled LSPs are related
                      to mesoscale convection over Western Europe and the
                      Mediterranean Sea $(18\%)$ and to tropical convection
                      $(8\%).$},
      cin          = {IEK-8},
      ddc          = {550},
      cid          = {I:(DE-Juel1)IEK-8-20101013},
      pnm          = {233 - Trace gas and aerosol processes in the troposphere
                      (POF2-233)},
      pid          = {G:(DE-HGF)POF2-233},
      typ          = {PUB:(DE-HGF)16},
      UT           = {WOS:000345425700001},
      doi          = {10.3402/tellusb.v66.25544},
      url          = {https://juser.fz-juelich.de/record/172736},
}