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@ARTICLE{Graf:1014226,
      author       = {Graf, Alexander and Wohlfahrt, Georg and Aranda-Barranco,
                      Sergio and Arriga, Nicola and Brümmer, Christian and
                      Ceschia, Eric and Ciais, Philippe and Desai, Ankur R. and Di
                      Lonardo, Sara and Gharun, Mana and Grünwald, Thomas and
                      Hörtnagl, Lukas and Kasak, Kuno and Klosterhalfen, Anne and
                      Knohl, Alexander and Kowalska, Natalia and Leuchner, Michael
                      and Lindroth, Anders and Mauder, Matthias and Migliavacca,
                      Mirco and Morel, Alexandra C. and Pfennig, Andreas and
                      Poorter, Hendrik and Terán, Christian Poppe and Reitz,
                      Oliver and Rebmann, Corinna and Sanchez-Azofeifa, Arturo and
                      Schmidt, Marius and Šigut, Ladislav and Tomelleri, Enrico
                      and Yu, Ke and Varlagin, Andrej and Vereecken, Harry},
      title        = {{J}oint optimization of land carbon uptake and albedo can
                      help achieve moderate instantaneous and long-term cooling
                      effects},
      journal      = {Communications earth $\&$ environment},
      volume       = {4},
      number       = {1},
      issn         = {2662-4435},
      address      = {London},
      publisher    = {Springer Nature},
      reportid     = {FZJ-2023-03210},
      pages        = {298},
      year         = {2023},
      abstract     = {Both carbon dioxide uptake and albedo of the land surface
                      affect global climate. However, climate change mitigation by
                      increasing carbon uptake can cause a warming trade-off by
                      decreasing albedo, with most research focusing on
                      afforestation and its interaction with snow. Here, we
                      present carbon uptake and albedo observations from 176
                      globally distributed flux stations. We demonstrate a gradual
                      decline in maximum achievable annual albedo as carbon uptake
                      increases, even within subgroups of non-forest and snow-free
                      ecosystems. Based on a paired-site permutation approach, we
                      quantify the likely impact of land use on carbon uptake and
                      albedo. Shifting to the maximum attainable carbon uptake at
                      each site would likely cause moderate net global warming for
                      the first approximately 20 years, followed by a strong
                      cooling effect. A balanced policy co-optimizing carbon
                      uptake and albedo is possible that avoids warming on any
                      timescale, but results in a weaker long-term cooling
                      effect.},
      cin          = {IBG-3},
      ddc          = {550},
      cid          = {I:(DE-Juel1)IBG-3-20101118},
      pnm          = {2173 - Agro-biogeosystems: controls, feedbacks and impact
                      (POF4-217) / TERENO - Terrestrial Environmental
                      Observatories (TERENO-2008)},
      pid          = {G:(DE-HGF)POF4-2173 / G:(DE-HGF)TERENO-2008},
      typ          = {PUB:(DE-HGF)16},
      UT           = {WOS:001054863600001},
      doi          = {10.1038/s43247-023-00958-4},
      url          = {https://juser.fz-juelich.de/record/1014226},
}