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@ARTICLE{Ng:835938,
      author       = {Ng, Nga Lee and Brown, Steven S. and Archibald, Alexander
                      T. and Atlas, Elliot and Cohen, Ronald C. and Crowley, John
                      N. and Day, Douglas A. and Donahue, Neil M. and Fry, Juliane
                      and Fuchs, Hendrik and Griffin, Robert J. and Guzman,
                      Marcelo I. and Herrmann, Hartmut and Hodzic, Alma and
                      Iinuma, Yoshiteru and Jimenez, José L. and Kiendler-Scharr,
                      Astrid and Lee, Ben H. and Luecken, Deborah J. and Mao,
                      Jingqiu and McLaren, Robert and Mutzel, Anke and Osthoff,
                      Hans D. and Ouyang, Bin and Picquet-Varrault, Benedicte and
                      Platt, Ulrich and Pye, Havala O. T. and Rudich, Yinon and
                      Schwantes, Rebecca H. and Shiraiwa, Manabu and Stutz, Jochen
                      and Thornton, Joel A. and Tilgner, Andreas and Williams,
                      Brent J. and Zaveri, Rahul A.},
      title        = {{N}itrate radicals and biogenic volatile organic compounds:
                      oxidation, mechanisms, and organic aerosol},
      journal      = {Atmospheric chemistry and physics},
      volume       = {17},
      number       = {3},
      issn         = {1680-7324},
      address      = {Katlenburg-Lindau},
      publisher    = {EGU},
      reportid     = {FZJ-2017-05070},
      pages        = {2103 - 2162},
      year         = {2017},
      abstract     = {Oxidation of biogenic volatile organic compounds (BVOC) by
                      the nitrate radical (NO3) represents one of the important
                      interactions between anthropogenic emissions related to
                      combustion and natural emissions from the biosphere. This
                      interaction has been recognized for more than 3 decades,
                      during which time a large body of research has emerged from
                      laboratory, field, and modeling studies. NO3-BVOC reactions
                      influence air quality, climate and visibility through
                      regional and global budgets for reactive nitrogen
                      (particularly organic nitrates), ozone, and organic aerosol.
                      Despite its long history of research and the significance of
                      this topic in atmospheric chemistry, a number of important
                      uncertainties remain. These include an incomplete
                      understanding of the rates, mechanisms, and organic aerosol
                      yields for NO3-BVOC reactions, lack of constraints on the
                      role of heterogeneous oxidative processes associated with
                      the NO3 radical, the difficulty of characterizing the
                      spatial distributions of BVOC and NO3 within the poorly
                      mixed nocturnal atmosphere, and the challenge of
                      constructing appropriate boundary layer schemes and
                      non-photochemical mechanisms for use in state-of-the-art
                      chemical transport and chemistry–climate models.},
      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},
      UT           = {WOS:000395106900002},
      pubmed       = {pmid:30147712},
      doi          = {10.5194/acp-17-2103-2017},
      url          = {https://juser.fz-juelich.de/record/835938},
}