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@ARTICLE{Robrecht:862200,
      author       = {Robrecht, Sabine and Vogel, Bärbel and Grooß, Jens-Uwe
                      and Rosenlof, Karen and Thornberry, Troy and Rollins, Andrew
                      and Krämer, Martina and Christensen, Lance and Müller,
                      Rolf},
      title        = {{M}echanism of ozone loss under enhanced water vapour
                      conditions in the mid-latitude lower stratosphere in summer},
      journal      = {Atmospheric chemistry and physics / Discussions Discussions
                      [...]},
      volume       = {-},
      issn         = {1680-7375},
      address      = {Katlenburg-Lindau},
      publisher    = {EGU},
      reportid     = {FZJ-2019-02548},
      pages        = {1 - 41},
      year         = {2019},
      abstract     = {Water vapour convectively injected into the mid-latitude
                      lowermost stratosphere could affect stratospheric ozone. The
                      associated potential ozone loss process requires low
                      temperatures and an elevated water vapour mixing ratio. An
                      increase in sulphate aerosol surface area due to a volcanic
                      eruption or geoengineering could increase the likelihood of
                      occurrence of this process. However, the chemical mechanism
                      of this ozone loss process has not yet been analysed in
                      sufficient detail and its sensitivity to various conditions
                      is not yet clear. Under conditions of climate change
                      associated with an increase in greenhouse gases, both a
                      stratospheric cooling and an increase in water vapour
                      convectively injected into the stratosphere is expected.
                      Understanding the influence of low temperatures, elevated
                      water vapour and enhanced sulphate particles on this ozone
                      loss mechanism is a key step in estimating the impact of
                      climate change and potential sulphate geoengineering on
                      mid-latitude ozone.},
      cin          = {IEK-7},
      ddc          = {550},
      cid          = {I:(DE-Juel1)IEK-7-20101013},
      pnm          = {244 - Composition and dynamics of the upper troposphere and
                      middle atmosphere (POF3-244)},
      pid          = {G:(DE-HGF)POF3-244},
      typ          = {PUB:(DE-HGF)16},
      doi          = {10.5194/acp-2018-1193},
      url          = {https://juser.fz-juelich.de/record/862200},
}