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@TECHREPORT{PoshyvailoStrube:1022224,
      author       = {Poshyvailo-Strube, Liubov and Niklas, Wagner and Furusho,
                      Carina and Hartick, Carl and Görgen, Klaus and Kollet,
                      Stefan},
      title        = {{G}roundwater in {T}errestrial {S}ystems {M}odelling over
                      {E}urope: {N}ew {H}eat {E}vents {C}limatology for
                      {H}istorical {T}ime {S}pan and {P}rojections},
      number       = {Final report 2022},
      reportid     = {FZJ-2024-01345, Final report 2022},
      pages        = {122-125},
      year         = {2022},
      abstract     = {The number of extreme hydroclimatic events (e.g., droughts,
                      heat waves, heavy precipitation) increased during the recent
                      years, and will likely occur even more often in the future
                      (e.g., Hari et al. 2020; Molina et al. 2020; IPCC, 2021),
                      resulting in multiple socio-economic impacts. In order to
                      develop useful adaptation strategies consistent,
                      high-resolution climate data are needed. The groundwater
                      (GW) representation in most regional climate models (RCMs)
                      is generally oversimplified or absent, as well as its
                      interaction with soil moisture and atmosphere, leading to
                      biases in simulation of extreme heat events. In fact, many
                      RCMs overestimate the heat waves frequency, duration and
                      intensity (e.g., Vautard et al. 2013; Lhotka et al. 2018).In
                      this project, we explicitly simulate full 3D soil and GW
                      dynamics, closing the terrestrial water cycle from GW across
                      the land surface into the atmosphere, by utilizing the
                      Terrestrial Systems Modelling Platform (TSMP) over the
                      EURO-CORDEX domain. We obtained all terrestrial essential
                      climate variables and indices for historical time span and
                      the climate change projections with the Representative
                      Concentration Pathways (RCP) 2.6 and RCP 8.5 (a rise in
                      global temperature by 1.5°C and 4°C by 2100 respectively).
                      Our analysis focused on the assessment of the effects of GW
                      on the evolution of heat waves by investigating its
                      frequency, duration and intensity.},
      cin          = {IBG-3},
      cid          = {I:(DE-Juel1)IBG-3-20101118},
      pnm          = {2173 - Agro-biogeosystems: controls, feedbacks and impact
                      (POF4-217) / 2A2 - HI-CAM (CARF - CCA) (POF4-2A2)},
      pid          = {G:(DE-HGF)POF4-2173 / G:(DE-HGF)POF4-2A2},
      typ          = {PUB:(DE-HGF)29},
      url          = {https://juser.fz-juelich.de/record/1022224},
}