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@ARTICLE{Lhnert:187197,
      author       = {Löhnert, U. and Schween, J. H. and Acquistapace, C. and
                      Ebell, K. and Maahn, M. and Barreraverdejo, M. and Hirsikko,
                      A. and Bohn, B. and Knaps, A. and O'connor, E. and Simmer,
                      C. and Wahner, A. and Crewell, S.},
      title        = {{JOYCE}: {J}uelich {O}bservatory for {C}loud {E}volution},
      journal      = {Bulletin of the American Meteorological Society},
      volume       = {96},
      number       = {7},
      issn         = {1520-0477},
      address      = {Boston, Mass.},
      publisher    = {ASM},
      reportid     = {FZJ-2015-00871},
      pages        = {1157–1174},
      year         = {2014},
      abstract     = {The Jülich Observatory for Cloud Evolution (JOYCE),
                      located at Forschungszentrum Jülich in the most western
                      part of Germany, is a recently established platform for
                      cloud research. The main objective of JOYCE is to provide
                      observations, which improve our understanding of the cloudy
                      boundary layer in a midlatitude environment. Continuous and
                      temporally highly resolved measurements that are
                      specifically suited to characterize the diurnal cycle of
                      water vapor, stability, and turbulence in the lower
                      troposphere are performed with a special focus on
                      atmosphere–surface interaction. In addition, instruments
                      are set up to measure the micro- and macrophysical
                      properties of clouds in detail and how they interact with
                      different boundary layer processes and the large-scale
                      synoptic situation. For this, JOYCE is equipped with an
                      array of state-of-the-art active and passive remote sensing
                      and in situ instruments, which are briefly described in this
                      scientific overview. As an example, a 24-h time series of
                      the evolution of a typical cumulus cloud-topped boundary
                      layer is analyzed with respect to stability, turbulence, and
                      cloud properties. Additionally, we present longer-term
                      statistics, which can be used to elucidate the diurnal cycle
                      of water vapor, drizzle formation through autoconversion,
                      and warm versus cold rain precipitation formation. Both case
                      studies and long-term observations are important for
                      improving the representation of clouds in climate and
                      numerical weather prediction models.},
      cin          = {IEK-8 / S-UM},
      ddc          = {550},
      cid          = {I:(DE-Juel1)IEK-8-20101013 / I:(DE-Juel1)S-UM-20090406},
      pnm          = {233 - Trace gas and aerosol processes in the troposphere
                      (POF2-233)},
      pid          = {G:(DE-HGF)POF2-233},
      typ          = {PUB:(DE-HGF)16},
      UT           = {WOS:000359855000001},
      doi          = {10.1175/BAMS-D-14-00105.1},
      url          = {https://juser.fz-juelich.de/record/187197},
}