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@ARTICLE{Han:872729,
      author       = {Han, Cunbo and Brdar, Slavko and Kollet, Stefan},
      title        = {{R}esponse of {C}onvective {B}oundary {L}ayer and {S}hallow
                      {C}umulus to {S}oil {M}oisture {H}eterogeneity: {A}
                      {L}arge‐{E}ddy {S}imulation {S}tudy},
      journal      = {Journal of advances in modeling earth systems},
      volume       = {11},
      number       = {12},
      issn         = {1942-2466},
      address      = {Fort Collins, Colo.},
      reportid     = {FZJ-2020-00207},
      pages        = {4305-4322},
      year         = {2019},
      abstract     = {In this study, the impact of varying soil moisture
                      heterogeneity (spatial variance and structure) on the
                      development of the convective boundary layer and shallow
                      cumulus clouds was investigated. Applying soil moisture
                      heterogeneity generated via spatially correlated Gaussian
                      random fields based on a power law model and idealized
                      atmospheric vertical profiles as initial conditions, three
                      sets of large‐eddy simulations provide insight in the
                      influence of soil moisture heterogeneity on the ensuing
                      growth of the convective boundary layer and development of
                      shallow cumulus clouds. A sensitivity on the strong, weak,
                      and unstructured soil moisture heterogeneity is
                      investigated. The simulation results show that
                      domain‐averaged land surface sensible heat and latent heat
                      flux change strongly with changing soil moisture variance
                      because of the interactions between surface heterogeneity
                      and induced circulations, while domain means of soil
                      moisture are identical. Vertical profiles of boundary layer
                      characteristics are strongly influenced by the surface
                      energy partitioning and induced circulations, especially the
                      profiles of liquid water and liquid water flux. The amount
                      of liquid water and liquid water flux increases with
                      increasing structure. In addition, the liquid water path is
                      higher in case of strongly‐structured heterogeneity
                      because more available energy is partitioned into latent
                      heat and more intensive updrafts exist. Interestingly, the
                      increase of liquid water path with increasing soil moisture
                      variance only occurs in the strongly structured cases, which
                      suggests that soil moisture variance and structure work
                      conjunctively in the surface energy partitioning and the
                      cloud formation.},
      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:000502179000001},
      doi          = {10.1029/2019MS001772},
      url          = {https://juser.fz-juelich.de/record/872729},
}