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@ARTICLE{Snider:10074,
      author       = {Snider, J.R. and Wex, H. and Rose, D. and Kristensson, A.
                      and Stratmann, F. and Henning, T. and Henning, S. and
                      Kiselev, A. and Bilde, M. and Burkhart, M. and Dusek, U. and
                      Frank, G.P. and Kiendler-Scharr, A. and Mentel, T. F. and
                      Petters, M.D. and Pöschl, U.},
      title        = {{I}ntercomparison of cloud condensation nuclei and
                      hygroscopic fraction the {LACIS} {E}xperiment in {N}ovember
                      ({LE}x{N}o)},
      journal      = {Journal of Geophysical Research},
      volume       = {115},
      issn         = {0148-0227},
      address      = {Washington, DC},
      publisher    = {Union},
      reportid     = {PreJuSER-10074},
      pages        = {D11205},
      year         = {2010},
      note         = {Several LExNo participants (G. Frank, A. Kiendler-Scharr,
                      A. Kristensson, T. F. Mentel, D. Rose, J. Snider, and S.
                      Walter) thank Atmospheric Composition Change: a European
                      Network (ACCENT) for travel support. M. Bilde thanks the
                      Nordic Center of Excellence, Research Unit BACCI, and Danish
                      Natural Science Research Council for financial support. As a
                      whole, the LExNo group thanks Simon Clegg. LExNo was hosted
                      by the research group in Leipzig; their efforts were
                      essential for bringing the study to fruition. The work of
                      three reviewers is also acknowledged.},
      abstract     = {Four cloud condensation nuclei (CCN) instruments were used
                      to sample size-selected particles prepared at the Leipzig
                      Aerosol Cloud Interaction Simulator facility. Included were
                      two Wyoming static diffusion CCN instruments, the continuous
                      flow instrument built by Droplet Measurement Technologies,
                      and the continuous flow Leipzig instrument. The aerosols
                      were composed of ammonium sulfate, levoglucosan,
                      levoglucosan and soot, and ammonium hydrogen sulfate and
                      soot. Comparisons are made among critical supersaturation
                      values from the CCN instruments and derived from
                      measurements made with a humidified tandem differential
                      mobility system. The comparison is quite encouraging: with
                      few exceptions the reported critical supersaturations agree
                      within known experimental uncertainty limits. Also reported
                      are CCN- and hygroscopicity-based estimates of the soot
                      particles' solute fraction. Relative differences between
                      these are as large as $40\%,$ but an error analysis
                      demonstrates that agreement within experimental uncertainty
                      is achieved. We also analyze data from the Droplet
                      Measurement Technologies and the two Wyoming static
                      diffusion instruments for evidence of size distribution
                      broadening and investigate levoglucosan particle growth
                      kinetics in the Wyoming CCN instrument.},
      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:000278453500003},
      doi          = {10.1029/2009JD012618},
      url          = {https://juser.fz-juelich.de/record/10074},
}