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@ARTICLE{Ploeger:838130,
      author       = {Ploeger, Felix and Konopka, Paul and Walker, Kaley and
                      Riese, Martin},
      title        = {{Q}uantifying pollution transport from the {A}sian monsoon
                      anticyclone into the lower stratosphere},
      journal      = {Atmospheric chemistry and physics},
      volume       = {17},
      number       = {11},
      issn         = {1680-7324},
      address      = {Katlenburg-Lindau},
      publisher    = {EGU},
      reportid     = {FZJ-2017-06834},
      pages        = {7055 - 7066},
      year         = {2017},
      abstract     = {Pollution transport from the surface to the stratosphere
                      within the Asian monsoon circulation may cause harmful
                      effects on stratospheric chemistry and climate. Here, we
                      investigate air mass transport from the monsoon anticyclone
                      into the stratosphere using a Lagrangian chemistry transport
                      model. We show how two main transport pathways from the
                      anticyclone emerge: (i) into the tropical stratosphere
                      (tropical pipe), and (ii) into the Northern Hemisphere (NH)
                      extratropical lower stratosphere. Maximum anticyclone air
                      mass fractions reach around $5 \%$ in the tropical pipe
                      and $15 \%$ in the extratropical lowermost stratosphere
                      over the course of a year. The anticyclone air mass fraction
                      correlates well with satellite hydrogen cyanide (HCN) and
                      carbon monoxide (CO) observations, confirming that pollution
                      is transported deep into the tropical stratosphere from the
                      Asian monsoon anticyclone. Cross-tropopause transport occurs
                      in a vertical chimney, but with the pollutants transported
                      quasi-horizontally along isentropes above the tropopause
                      into the tropics and NH.},
      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:000403219000006},
      doi          = {10.5194/acp-17-7055-2017},
      url          = {https://juser.fz-juelich.de/record/838130},
}