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@ARTICLE{Tilmes:901808,
      author       = {Tilmes, S. and Richter, J. H. and Kravitz, B. and
                      MacMartin, D. G. and Glanville, A. S. and Visioni, D. and
                      Kinnison, D. E. and Müller, R.},
      title        = {{S}ensitivity of {T}otal {C}olumn {O}zone to
                      {S}tratospheric {S}ulfur {I}njection {S}trategies},
      journal      = {Geophysical research letters},
      volume       = {48},
      number       = {19},
      issn         = {1944-8007},
      address      = {Hoboken, NJ},
      publisher    = {Wiley},
      reportid     = {FZJ-2021-03832},
      pages        = {e2021GL094058},
      year         = {2021},
      abstract     = {We explore the impact of different stratospheric sulfur
                      injection strategies to counter greenhouse gas induced
                      warming on total column ozone (TCO), including high and low
                      altitude injections at four latitudes, equatorial
                      injections, and using a configuration with higher vertical
                      resolution, based on a state-of-the-art Earth system model.
                      The experiments maintain global surface temperatures at 2020
                      conditions, while following the unmitigated future scenario.
                      Within the first 10 years of the injection, we find an
                      abrupt deepening of the Antarctic ozone hole by $8\%–20\%$
                      and changes up to $5\%$ for other regions and seasons. The
                      ozone hole recovery is delayed by ∼25 to over 55 years,
                      with the fastest recovery for low-altitude injections and
                      slowest for equatorial injections. Mid to high-latitude TCO
                      increases by $15\%$ in Northern Hemisphere winter and spring
                      between 2010–2019 and 2080–2089 due to both increasing
                      greenhouse gases and increasing sulfur injections.
                      Implications for ecosystems need to be investigated.},
      cin          = {IEK-7},
      ddc          = {550},
      cid          = {I:(DE-Juel1)IEK-7-20101013},
      pnm          = {2112 - Climate Feedbacks (POF4-211)},
      pid          = {G:(DE-HGF)POF4-2112},
      typ          = {PUB:(DE-HGF)16},
      UT           = {WOS:000706306000026},
      doi          = {10.1029/2021GL094058},
      url          = {https://juser.fz-juelich.de/record/901808},
}