% 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{Vereecken:909014,
      author       = {Vereecken, Harry and Amelung, Wulf and Bauke, Sara L. and
                      Bogena, Heye and Brüggemann, Nicolas and Montzka, Carsten
                      and Vanderborght, Jan and Bechtold, Michel and Blöschl,
                      Günter and Carminati, Andrea and Javaux, Mathieu and
                      Konings, Alexandra G. and Kusche, Jürgen and Neuweiler,
                      Insa and Or, Dani and Steele-Dunne, Susan and Verhoef, Anne
                      and Young, Michael and Zhang, Yonggen},
      title        = {{S}oil hydrology in the {E}arth system},
      journal      = {Nature reviews},
      volume       = {3},
      issn         = {2662-138X},
      address      = {London},
      publisher    = {Nature Research},
      reportid     = {FZJ-2022-02952},
      pages        = {573–587},
      year         = {2022},
      note         = {Kein Post-print vorhanden},
      abstract     = {Soil hydrological processes (SHP) support ecosystems,
                      modulate the impact of climate change on terrestrial systems
                      and control feedback mechanisms between water, energy and
                      biogeochemical cycles. However, land-use changes and extreme
                      events are increasingly impacting these processes. In this
                      Review, we describe SHP across scales and examine their
                      links with soil properties, ecosystem processes and climate.
                      Soil structure influences SHP such as infiltration, soil
                      water redistribution and root water uptake on small scales.
                      On local scales, SHP are driven by root water uptake,
                      vegetation and groundwater dynamics. Regionally, SHP are
                      impacted by extreme events such as droughts, floods,
                      heatwaves and land-use change; however, antecedent and
                      current SHP partially determine the broader effects of
                      extreme events. Emerging technologies such as wireless and
                      automated sensing, soil moisture observation through novel
                      synthetic aperture radars satellites, big data analysis and
                      machine learning approaches offer unique opportunities to
                      advance soil hydrology. These advances, in tandem with the
                      inclusion of more key soil types and properties in models,
                      will be pivotal in predicting the role of SHP during global
                      change.},
      cin          = {IBG-3},
      ddc          = {570},
      cid          = {I:(DE-Juel1)IBG-3-20101118},
      pnm          = {2173 - Agro-biogeosystems: controls, feedbacks and impact
                      (POF4-217)},
      pid          = {G:(DE-HGF)POF4-2173},
      typ          = {PUB:(DE-HGF)16},
      UT           = {WOS:000836416900002},
      doi          = {10.1038/s43017-022-00324-6},
      url          = {https://juser.fz-juelich.de/record/909014},
}