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@ARTICLE{Macke:829416,
      author       = {Macke, Andreas and Seifert, Patric and Baars, Holger and
                      Barthlott, Christian and Beekmans, Christoph and Behrendt,
                      Andreas and Bohn, Birger and Brueck, Matthias and Bühl,
                      Johannes and Crewell, Susanne and Damian, Thomas and Deneke,
                      Hartwig and Düsing, Sebastian and Foth, Andreas and Di
                      Girolamo, Paolo and Hammann, Eva and Heinze, Rieke and
                      Hirsikko, Anne and Kalisch, John and Kalthoff, Norbert and
                      Kinne, Stefan and Kohler, Martin and Löhnert, Ulrich and
                      Madhavan, Bomidi Lakshmi and Maurer, Vera and Muppa, Shravan
                      Kumar and Schween, Jan and Serikov, Ilya and Siebert, Holger
                      and Simmer, Clemens and Späth, Florian and Steinke, Sandra
                      and Träumner, Katja and Trömel, Silke and Wehner, Birgit
                      and Wieser, Andreas and Wulfmeyer, Volker and Xie, Xinxin},
      title        = {{T}he {HD}({CP})2 {O}bservational {P}rototype {E}xperiment
                      ({HOPE}) – an overview},
      journal      = {Atmospheric chemistry and physics},
      volume       = {17},
      number       = {7},
      issn         = {1680-7324},
      address      = {Katlenburg-Lindau},
      publisher    = {EGU},
      reportid     = {FZJ-2017-03120},
      pages        = {4887 - 4914},
      year         = {2017},
      abstract     = {The HD(CP)2 Observational Prototype Experiment (HOPE) was
                      performed as a major 2-month field experiment in Jülich,
                      Germany, in April and May 2013, followed by a smaller
                      campaign in Melpitz, Germany, in September 2013. HOPE has
                      been designed to provide an observational dataset for a
                      critical evaluation of the new German community atmospheric
                      icosahedral non-hydrostatic (ICON) model at the scale of the
                      model simulations and further to provide information on
                      land-surface–atmospheric boundary layer exchange, cloud
                      and precipitation processes, as well as sub-grid variability
                      and microphysical properties that are subject to
                      parameterizations. HOPE focuses on the onset of clouds and
                      precipitation in the convective atmospheric boundary layer.
                      This paper summarizes the instrument set-ups, the intensive
                      observation periods, and example results from both
                      campaigns.HOPE-Jülich instrumentation included a radio
                      sounding station, 4 Doppler lidars, 4 Raman lidars (3 of
                      them provide temperature, 3 of them water vapour, and all of
                      them particle backscatter data), 1 water vapour differential
                      absorption lidar, 3 cloud radars, 5 microwave radiometers, 3
                      rain radars, 6 sky imagers, 99 pyranometers, and 5 sun
                      photometers operated at different sites, some of them in
                      synergy. The HOPE-Melpitz campaign combined ground-based
                      remote sensing of aerosols and clouds with helicopter- and
                      balloon-based in situ observations in the atmospheric column
                      and at the surface.HOPE provided an unprecedented collection
                      of atmospheric dynamical, thermodynamical, and micro- and
                      macrophysical properties of aerosols, clouds, and
                      precipitation with high spatial and temporal resolution
                      within a cube of approximately
                      10  ×  10  ×  10 km3. HOPE data will
                      significantly contribute to our understanding of boundary
                      layer dynamics and the formation of clouds and
                      precipitation. The datasets have been made available through
                      a dedicated data portal.First applications of HOPE data for
                      model evaluation have shown a general agreement between
                      observed and modelled boundary layer height, turbulence
                      characteristics, and cloud coverage, but they also point to
                      significant differences that deserve further investigations
                      from both the observational and the modelling perspective.},
      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:000403956400004},
      doi          = {10.5194/acp-17-4887-2017},
      url          = {https://juser.fz-juelich.de/record/829416},
}