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@ARTICLE{Vogel:155472,
      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 {N}orthern {E}urope: rapid uplift in typhoons and
                      eastward eddy shedding of the {A}sian monsoon anticyclone2},
      journal      = {Atmospheric chemistry and physics / Discussions},
      volume       = {14},
      number       = {12},
      issn         = {1680-7375},
      address      = {Katlenburg-Lindau},
      publisher    = {EGU},
      reportid     = {FZJ-2014-04638},
      pages        = {18461 - 18497},
      year         = {2014},
      abstract     = {During the TACTS aircraft campaign 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. The
                      measurements indicate that these air masses 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. Afterwards
                      they are injected directly into 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
                      find that the combination of rapid uplift by a typhoon and
                      eastward eddy shedding from the Asian monsoon anticyclone is
                      an additional fast transport pathway that, in this study,
                      carries 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},
      doi          = {10.5194/acpd-14-18461-2014},
      url          = {https://juser.fz-juelich.de/record/155472},
}