% 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{Han:840426,
      author       = {Han, Cunbo and Ma, Yaoming and Chen, Xuelong and Su,
                      Zhongbo},
      title        = {{T}rends of land surface heat fluxes on the {T}ibetan
                      {P}lateau from 2001 to 2012},
      journal      = {International journal of climatology},
      volume       = {37},
      number       = {14},
      issn         = {0899-8418},
      address      = {Chichester [u.a.]},
      publisher    = {Wiley},
      reportid     = {FZJ-2017-07943},
      pages        = {4757 - 4767},
      year         = {2017},
      abstract     = {A parameterization approach of effective roughness length
                      was introduced into the Surface Energy Balance System (SEBS)
                      model to account for subgrid-scale topographical influences.
                      Regional distribution of land surface heat flux values
                      (including net radiation flux, ground heat flux, sensible
                      heat flux, and latent heat flux) was estimated on the
                      Tibetan Plateau (TP) based on the SEBS model, and utilizing
                      remote sensing products and reanalysis datasets. We then
                      investigated annual trends in these fluxes for the period
                      2001–2012. It was found that land surface net radiation
                      flux increased slightly, especially in high, mountainous
                      regions and the central TP, and was influenced by glacial
                      retreat and topsoil wetting, respectively. Sensible heat
                      flux decreased overall, especially in the central and
                      northern TP. In the Yarlung Zangbo River (YZR) Basin, the
                      sensible heat flux increased because of a rise in the
                      ground-air temperature difference. The latent heat flux
                      increased over the majority TP, except for areas in the YZR
                      Basin. This can be attributed to increases in precipitation
                      and vegetation greening.},
      cin          = {IBG-3},
      ddc          = {550},
      cid          = {I:(DE-Juel1)IBG-3-20101118},
      pnm          = {255 - Terrestrial Systems: From Observation to Prediction
                      (POF3-255)},
      pid          = {G:(DE-HGF)POF3-255},
      typ          = {PUB:(DE-HGF)16},
      UT           = {WOS:000414322800001},
      doi          = {10.1002/joc.5119},
      url          = {https://juser.fz-juelich.de/record/840426},
}