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@ARTICLE{MllmannCoers:34285,
      author       = {Möllmann-Coers, M. and Klemp, D. and Mannschreck, K. and
                      Slemr, E. C.},
      title        = {{D}etermination of anthropogenic emissions in the
                      {A}ugsburg area by the source-tracer-ratio method},
      journal      = {Atmospheric environment},
      volume       = {36},
      issn         = {1352-2310},
      address      = {Amsterdam [u.a.]},
      publisher    = {Elsevier Science},
      reportid     = {PreJuSER-34285},
      pages        = {95 - 107},
      year         = {2002},
      note         = {Record converted from VDB: 12.11.2012},
      abstract     = {Air-quality models require as input emission inventories of
                      individual compounds high temporal and spatial resolution.
                      These emission inventories are calculated by complex
                      emission models. To evaluate these models, emission rates of
                      CO and NO, of the city of Augsburg were determined in March
                      and October using two independent methods and were compared
                      with emission rates calculated by an emission model. This
                      paper outlines the source-tracer-ratio (STR) method,
                      describes its implementation in Augsburg, and presents the
                      results obtained in four successful experiments. The CO
                      emission rate was derived directly from the STR method,
                      whereas the NO, emission rate is calculated from the CO
                      emission rate using the average CO/NOx correlation in the
                      city plume from the long-term dataset obtained within the
                      Augsburg experiment. The CO and NO, emission rates obtained
                      on 10, 22, and 23 October 1998, were in reasonable agreement
                      with emission rates determined by a mass balance method. The
                      CO emission rate on 23 March 1998, was about twice as large
                      as the autumn emission rates. This observation is consistent
                      with the observed mean emission ratios in March and October
                      obtained from long-term measurements. The CO emission rates
                      were also used to calculate absolute emission rates for a
                      number of hydrocarbons. (C) 2002 Elsevier Science Ltd. All
                      rights reserved.},
      keywords     = {J (WoSType)},
      cin          = {ICG-II / S},
      ddc          = {550},
      cid          = {I:(DE-Juel1)VDB48 / I:(DE-Juel1)VDB224},
      pnm          = {Chemie und Dynamik der Geo-Biosphäre},
      pid          = {G:(DE-Juel1)FUEK257},
      shelfmark    = {Environmental Sciences / Meteorology $\&$ Atmospheric
                      Sciences},
      typ          = {PUB:(DE-HGF)16},
      UT           = {WOS:000177154100008},
      url          = {https://juser.fz-juelich.de/record/34285},
}