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@ARTICLE{Reeves:34366,
      author       = {Reeves, C. E. and Penkett, S. A. and Bauguitte, S. and Law,
                      K. S. and Evans, M. J. and Bandy, B. J. and Monks, P. S. and
                      Edwards, G. D. and Philips, G. and Barjat, H. and Kent, J.
                      and Dewey, K. and Schmitgen, S. and Kley, D.},
      title        = {{P}otential for photochemical ozone formation in the
                      troposhere over the {N}orth {A}tlantic as derived from
                      aircraft observations during {ACSOE}},
      journal      = {Journal of Geophysical Research},
      volume       = {107},
      issn         = {0148-0227},
      address      = {Washington, DC},
      publisher    = {Union},
      reportid     = {PreJuSER-34366},
      pages        = {4707},
      year         = {2002},
      note         = {Record converted from VDB: 12.11.2012},
      abstract     = {[1] In this paper, ozone (O-3), water vapor (H2O), carbon
                      monoxide (CO), and peroxide concentrations and photolysis
                      rates measured in the troposphere over the North Atlantic
                      during two Atmospheric Chemistry Studies in the Oceanic
                      Environment (ACSOE) aircraft field campaigns are used to
                      calculate the concentration of nitric oxide (NO) required
                      for net photochemical O-3 production (nP(O3)) to be positive
                      (NOcomp). NOcomp tended to show a decrease with altitude,
                      although it was sometimes found to be low in the marine
                      boundary layer (MBL) where H2O concentrations were high and
                      O-3 concentrations were low. nP(O3) was calculated for the
                      spring when NO data were available and was found to be
                      mostly negative and generally increased from about -0.5 to
                      -0.2 ppbv hr(-1) in the MBL to +0.04 ppbv hr(-1) at about
                      7-8 km altitude. The results suggest that much of the lower
                      and middle troposphere over the eastern North Atlantic
                      during spring is in a state of slow net photochemical O-3
                      destruction. However, in the upper troposphere, the system
                      changes to one of net photochemical production, which
                      results from the drier environment and higher NO
                      concentrations. Furthermore, examples of net O-3 production
                      were also observed in the lower and middle troposphere
                      associated with either in situ sources of NO or long-range
                      transport of pollution. The paper also illustrates the
                      sensitivity of this O-3 production/loss state to H2O and NO
                      concentrations, photolysis rates, and temperatures.},
      keywords     = {J (WoSType)},
      cin          = {ICG-II},
      ddc          = {550},
      cid          = {I:(DE-Juel1)VDB48},
      pnm          = {Chemie und Dynamik der Geo-Biosphäre},
      pid          = {G:(DE-Juel1)FUEK257},
      shelfmark    = {Meteorology $\&$ Atmospheric Sciences},
      typ          = {PUB:(DE-HGF)16},
      UT           = {WOS:000181113600008},
      doi          = {10.1029/2002JD002415},
      url          = {https://juser.fz-juelich.de/record/34366},
}