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@ARTICLE{Baatz:894364,
      author       = {Baatz, R. and Franssen, H. J. Hendricks and Euskirchen, E.
                      and Sihi, D. and Dietze, M. and Ciavatta, S. and Fennel, K.
                      and Beck, H. and De Lannoy, G. and Pauwels, V. R. N. and
                      Raiho, A. and Montzka, C. and Williams, M. and Mishra, U.
                      and Poppe, C. and Zacharias, S. and Lausch, A. and
                      Samaniego, L. and Van Looy, K. and Bogena, H. and Adamescu,
                      M. and Mirtl, M. and Fox, A. and Goergen, K. and Naz, B. S.
                      and Zeng, Y. and Vereecken, H.},
      title        = {{R}eanalysis in {E}arth {S}ystem {S}cience: {T}owards
                      {T}errestrial {E}cosystem {R}eanalysis},
      journal      = {Reviews of geophysics},
      volume       = {715},
      issn         = {1944-9208},
      address      = {Hoboken, NJ},
      publisher    = {Wiley},
      reportid     = {FZJ-2021-03199},
      pages        = {1},
      year         = {2021},
      abstract     = {A reanalysis is a physically consistent set of optimally
                      merged simulated model states and historical observational
                      data, using data assimilation. High computational costs for
                      modelled processes and assimilation algorithms has led to
                      Earth system specific reanalysis products for the
                      atmosphere, the ocean and the land separately. Recent
                      developments include the advanced uncertainty quantification
                      and the generation of biogeochemical reanalysis for land and
                      ocean. Here, we review atmospheric and oceanic reanalyses,
                      and more in detail biogeochemical ocean and terrestrial
                      reanalyses. In particular, we identify land surface,
                      hydrologic and carbon cycle reanalyses which are nowadays
                      produced in targeted projects for very specific purposes.
                      Although a future joint reanalysis of land surface,
                      hydrologic and carbon processes represents an analysis of
                      important ecosystem variables, biotic ecosystem variables
                      are assimilated only to a very limited extent. Continuous
                      data sets of ecosystem variables are needed to explore
                      biotic-abiotic interactions and the response of ecosystems
                      to global change. Based on the review of existing
                      achievements, we identify five major steps required to
                      develop terrestrial ecosystem reanalysis to deliver
                      continuous data streams on ecosystem dynamics.},
      cin          = {IBG-3},
      ddc          = {550},
      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:000702346500001},
      doi          = {10.1029/2020RG000715},
      url          = {https://juser.fz-juelich.de/record/894364},
}