% IMPORTANT: The following is UTF-8 encoded.  This means that in the presence
% of non-ASCII characters, it will not work with BibTeX 0.99 or older.
% Instead, you should use an up-to-date BibTeX implementation like “bibtex8” or
% “biber”.

@ARTICLE{Eder:172290,
      author       = {Eder, Fabian and Schmidt, Marius and Damian, Thomas and
                      Träumner, Katja and Mauder, Matthias},
      title        = {{M}eso-scale eddies affect near-surface turbulent exchange:
                      evidence from lidar and tower measurements},
      journal      = {Journal of applied meteorology and climatology},
      volume       = {54},
      number       = {1},
      issn         = {1558-8432},
      address      = {Boston, Mass.},
      publisher    = {AMS},
      reportid     = {FZJ-2014-05773},
      pages        = {189-206},
      year         = {2015},
      abstract     = {The eddy-covariance technique tends to underestimate
                      turbulent heat fluxes, which results in nonclosure of the
                      surface energy balance. This study shows experimental
                      evidence that mesoscale turbulent organized structures,
                      which are inherently not captured by the standard
                      eddy-covariance technique, can affect near-surface turbulent
                      exchange. By using a combined setup of three Doppler wind
                      lidars above a cropland-dominated area in Germany,
                      low-frequency turbulent structures were detected in the
                      surface layer down to a few meters above ground. In
                      addition, data from two micrometeorological stations in the
                      study area were analyzed with respect to energy balance
                      closure. In accordance with several previous studies, the
                      data confirm a strong friction velocity dependence of the
                      energy balance residual. At both stations, the energy
                      balance residual was found to be positively correlated with
                      the vertical moisture gradient in the lower atmospheric
                      boundary layer, but at only one station was it correlated
                      with the temperature gradient. This result indicates that
                      mesoscale transport probably contributes more to the latent
                      heat flux than to the sensible heat flux, but this
                      conclusion depends largely on the measurement site.
                      Moreover, flow distortion due to tower mountings and
                      measurement devices affects the energy balance closure
                      considerably for certain wind directions.},
      cin          = {IBG-3},
      ddc          = {550},
      cid          = {I:(DE-Juel1)IBG-3-20101118},
      pnm          = {255 - Terrestrial Systems: From Observation to Prediction
                      (POF3-255) / TERENO - Terrestrial Environmental
                      Observatories (TERENO-2008) / 255 - Terrestrial Systems:
                      From Observation to Prediction (POF3-255) / DFG project
                      15232683 - TRR 32: Muster und Strukturen in
                      Boden-Pflanzen-Atmosphären-Systemen: Erfassung,
                      Modellierung und Datenassimilation (15232683)},
      pid          = {G:(DE-HGF)POF3-255 / G:(DE-HGF)TERENO-2008 /
                      G:(DE-HGF)POF3-255 / G:(GEPRIS)15232683},
      typ          = {PUB:(DE-HGF)16},
      UT           = {WOS:000347953700013},
      doi          = {10.1175/JAMC-D-14-0140.1},
      url          = {https://juser.fz-juelich.de/record/172290},
}