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@ARTICLE{Kloss:866364,
      author       = {Kloss, Corinna and Berthet, Gwenaël and Sellitto, Pasquale
                      and Ploeger, Felix and Bucci, Silvia and Khaykin, Sergey and
                      Jégou, Fabrice and Taha, Ghassan and Thomason, Larry W. and
                      Barret, Brice and Le Flochmoen, Eric and von Hobe, Marc and
                      Bossolasco, Adriana and Bègue, Nelson and Legras, Bernard},
      title        = {{T}ransport of the 2017 {C}anadian wildfire plume to the
                      tropics via the {A}sian monsoon circulation},
      journal      = {Atmospheric chemistry and physics},
      volume       = {19},
      number       = {21},
      issn         = {1680-7324},
      address      = {Katlenburg-Lindau},
      publisher    = {EGU},
      reportid     = {FZJ-2019-05520},
      pages        = {13547 - 13567},
      year         = {2019},
      abstract     = {We show that a fire plume injected into the lower
                      stratosphere at high northern latitudes during the Canadian
                      wildfire event in August 2017 partly reached the tropics.
                      The transport to the tropics was mediated by the
                      anticyclonic flow of the Asian monsoon circulation. The fire
                      plume reached the Asian monsoon area in late August/early
                      September, when the Asian monsoon anticyclone (AMA) was
                      still in place. While there is no evidence of mixing into
                      the center of the AMA, we show that a substantial part of
                      the fire plume is entrained into the anticyclonic flow at
                      the AMA edge and is transported from the extratropics to the
                      tropics, and possibly the Southern Hemisphere particularly
                      following the north–south flow on the eastern side of the
                      AMA. In the tropics the fire plume is lifted by ∼5 km in
                      7 months. Inside the AMA we find evidence of the Asian
                      tropopause aerosol layer (ATAL) in August, doubling
                      background aerosol conditions with a calculated top of the
                      atmosphere shortwave radiative forcing of
                      −0.05 W m−2. The regional climate impact of the fire
                      signal in the wider Asian monsoon area in September exceeds
                      the impact of the ATAL by a factor of 2–4 and compares to
                      that of a plume coming from an advected moderate volcanic
                      eruption. The stratospheric, trans-continental transport of
                      this plume to the tropics and the related regional climate
                      impact point to the importance of long-range dynamical
                      interconnections of pollution sources.},
      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:000496543000002},
      doi          = {10.5194/acp-19-13547-2019},
      url          = {https://juser.fz-juelich.de/record/866364},
}