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@ARTICLE{Wu:1002267,
      author       = {Wu, Xue and Qiao, Qi and Chen, Bing and Wang, Xin and
                      Hoffmann, Lars and Griessbach, Sabine and Tian, Yufang and
                      Wang, Yinan},
      title        = {{T}he influence of the {A}sian summer monsoon on volcanic
                      aerosol transport in the {UTLS} region},
      journal      = {npj climate and atmospheric science},
      volume       = {6},
      number       = {1},
      issn         = {2397-3722},
      address      = {London},
      publisher    = {Springer Nature},
      reportid     = {FZJ-2023-01249},
      pages        = {11},
      year         = {2023},
      abstract     = {This study analyses the influence of the Asian summer
                      monsoon on volcanic aerosol transport. Realistic,
                      altitude-resolved SO2 emissions of a middle-latitude
                      volcanic eruption (Sarychev 2009) and a tropical volcanic
                      eruption (Nabro 2011) were retrieved and used to initialize
                      the simulations of the long-range transport and dispersion
                      of the sulfate aerosol plumes. The barrier effect of the
                      Asian summer monsoon anticyclone (ASMA) isolated the
                      Sarychev eruption plume outside of the ASMA but constrained
                      the Nabro eruption plume inside of the ASMA, which is most
                      evident in the UTLS region between isotropic surfaces of
                      360–420 K. Meanwhile, the ASMA could transport a
                      fraction of the plume outside of ASMA quasi-horizontally to
                      the tropical tropopause layer along the southeastern
                      periphery of the anticyclonic circulation, and lift the
                      volcanic plume inside the ASMA anticyclonically across the
                      tropopause with an ascent rate of approximately 0.8 K/day.
                      By enhancing the meridional transport in the UTLS region and
                      lifting volcanic aerosols across the tropopause, the ASMA
                      significantly expanded the potential effects of volcanic
                      eruptions.},
      cin          = {JSC},
      ddc          = {530},
      cid          = {I:(DE-Juel1)JSC-20090406},
      pnm          = {5111 - Domain-Specific Simulation $\&$ Data Life Cycle Labs
                      (SDLs) and Research Groups (POF4-511) / DFG project
                      410579391 - Transportwege für Aerosol und Spurengase im
                      Asiatischen Monsun in der oberen Troposphäre und unteren
                      Stratosphäre (AeroTrac) (410579391)},
      pid          = {G:(DE-HGF)POF4-5111 / G:(GEPRIS)410579391},
      typ          = {PUB:(DE-HGF)16},
      UT           = {WOS:000936243600001},
      doi          = {10.1038/s41612-023-00339-w},
      url          = {https://juser.fz-juelich.de/record/1002267},
}