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@ARTICLE{Diallo:838417,
      author       = {Diallo, M. and Ploeger, F. and Konopka, P. and Birner, T.
                      and Müller, R. and Riese, M. and Garny, H. and Legras, B.
                      and Ray, E. and Berthet, G. and Jegou, F.},
      title        = {{S}ignificant contributions of volcanic aerosols to decadal
                      changes in the stratospheric circulation},
      journal      = {Geophysical research letters},
      volume       = {44},
      number       = {20},
      issn         = {0094-8276},
      address      = {Hoboken, NJ},
      publisher    = {Wiley},
      reportid     = {FZJ-2017-07026},
      pages        = {10,780–10,791},
      year         = {2017},
      abstract     = {The stratospheric circulation is an important element of
                      climate as it determines the concentration of radiatively
                      active species like water vapour and aerosol above the
                      tropopause. Climate models predict that increasing
                      greenhouse gas levels speed up the stratospheric
                      circulation. However, these results have been challenged by
                      observational estimates of the circulation strength,
                      constituting an uncertainty in current climate simulations.
                      Here, we quantify the effect of volcanic aerosol on the
                      stratospheric circulation focussing on the Mt. Pinatubo
                      eruption and discussing further the minor extratropical
                      volcanic eruptions after 2008. We show that the observed
                      pattern of decadal circulation change over the past decades
                      is substantially driven by volcanic aerosol injections.
                      Thus, climate model simulations need to realistically take
                      into account the effect of volcanic eruptions, including the
                      minor eruptions after 2008, for a reliable reproduction of
                      observed stratospheric circulation changes.},
      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},
      UT           = {WOS:000416761600080},
      doi          = {10.1002/2017GL074662},
      url          = {https://juser.fz-juelich.de/record/838417},
}