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@ARTICLE{Vogel:185575,
      author       = {Vogel, B. and Günther, G. and Müller, Rolf and Grooß,
                      J.-U. and Hoor, P. and Krämer, M. and Müller, S. and Zahn,
                      A. and Riese, M.},
      title        = {{F}ast transport from {S}outheast {A}sia boundary layer
                      sources to northern {E}urope: rapid uplift in typhoons and
                      eastward eddy shedding of the {A}sian monsoon anticyclone},
      journal      = {Atmospheric chemistry and physics},
      volume       = {14},
      number       = {23},
      issn         = {1680-7324},
      address      = {Katlenburg-Lindau},
      publisher    = {EGU},
      reportid     = {FZJ-2014-07001},
      pages        = {12745 - 12762},
      year         = {2014},
      abstract     = {Enhanced tropospheric trace gases such as CO, CH4 and H2O
                      and reduced stratospheric O3 were measured in situ in the
                      lowermost stratosphere over northern Europe on 26 September
                      2012 during the TACTS aircraft campaign. The measurements
                      indicate that these air masses clearly differ from the
                      stratospheric background. The calculation of 40-day backward
                      trajectories with the trajectory module of the CLaMS model
                      shows that these air masses are affected by the Asian
                      monsoon anticyclone. Some air masses originate from the
                      boundary layer in Southeast Asia/West Pacific and are
                      rapidly lifted (1–2 days) within a typhoon up to the outer
                      edge of the Asian monsoon anticyclone. Afterwards, the air
                      parcels are entrained by the anticyclonic circulation of the
                      Asian monsoon. The subsequent long-range transport (8–14
                      days) of enhanced water vapour and pollutants to the
                      lowermost stratosphere in northern Europe is driven by
                      eastward transport of tropospheric air from the Asian
                      monsoon anticyclone caused by an eddy shedding event. We
                      found that the combination of rapid uplift by a typhoon and
                      eastward eddy shedding from the Asian monsoon anticyclone is
                      a novel fast transport pathway that may carry boundary
                      emissions from Southeast Asia/West Pacific within
                      approximately 5 weeks to the lowermost stratosphere in
                      northern Europe.},
      cin          = {IEK-7},
      ddc          = {550},
      cid          = {I:(DE-Juel1)IEK-7-20101013},
      pnm          = {234 - Composition and Dynamics of the Upper Troposphere and
                      Stratosphere (POF2-234)},
      pid          = {G:(DE-HGF)POF2-234},
      typ          = {PUB:(DE-HGF)16},
      UT           = {WOS:000346140100009},
      doi          = {10.5194/acp-14-12745-2014},
      url          = {https://juser.fz-juelich.de/record/185575},
}