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@ARTICLE{Tao:203188,
      author       = {Tao, Mengchu and Konopka, Paul and Ploeger, Felix and
                      Riese, Martin and Müller, Rolf and Volk, C. Michael},
      title        = {{I}mpact of stratospheric major warmings and the
                      quasi-biennial oscillation on the variability of
                      stratospheric water vapompo},
      journal      = {Geophysical research letters},
      volume       = {42},
      number       = {11},
      issn         = {0094-8276},
      address      = {Hoboken, NJ},
      publisher    = {Wiley},
      reportid     = {FZJ-2015-05189},
      pages        = {4599 - 4607},
      year         = {2015},
      abstract     = {Based on simulations with the Chemical Lagrangian Model of
                      the Stratosphere for the 1979–2013 period, driven by the
                      European Centre for Medium-Range Weather Forecasts
                      ERA-Interim reanalysis, we analyze the impact of the
                      quasi-biennial oscillation (QBO) and of Major Stratospheric
                      Warmings (MWs) on the amount of water vapor entering the
                      stratosphere during boreal winter. The amplitude of H2O
                      variation related to the QBO amounts to 0.5 ppmv. The
                      additional effect of MWs reaches its maximum about
                      2–4 weeks after the central date of the MW and strongly
                      depends on the QBO phase. Whereas during the easterly QBO
                      phase there is a pronounced drying of about 0.3 ppmv about
                      3 weeks after the MW, the impact of the MW during the
                      westerly QBO phase is smaller (about 0.2 ppmv) and more
                      diffusely spread over time. We suggest that the
                      MW-associated enhanced dehydration combined with a higher
                      frequency of MWs after the year 2000 may have contributed to
                      the lower stratospheric water vapor after 2000.},
      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) / HITEC - Helmholtz
                      Interdisciplinary Doctoral Training in Energy and Climate
                      Research (HITEC) (HITEC-20170406)},
      pid          = {G:(DE-HGF)POF3-244 / G:(DE-Juel1)HITEC-20170406},
      typ          = {PUB:(DE-HGF)16},
      UT           = {WOS:000357511200043},
      doi          = {10.1002/2015GL064443},
      url          = {https://juser.fz-juelich.de/record/203188},
}