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@ARTICLE{Klingmller:858148,
      author       = {Klingmüller, Klaus and Lelieveld, Jos and Karydis, Vlassis
                      and Stenchikov, Georgiy L.},
      title        = {{D}irect radiative effect of dust-pollution interactions},
      journal      = {Atmospheric chemistry and physics / Discussions Discussions
                      [...]},
      volume       = {1104},
      issn         = {1680-7375},
      address      = {Katlenburg-Lindau},
      publisher    = {EGU},
      reportid     = {FZJ-2018-07055},
      pages        = {1 - 20},
      year         = {2018},
      abstract     = {The chemical ageing of aeolian dust, through interactions
                      with air pollution, affects the optical and hygroscopic
                      properties of the mineral particles and hence their
                      atmospheric residence time and climate forcing. Conversely,
                      the chemical composition of the dust particles and their
                      role as coagulation partners impact the abundance of
                      particulate air pollution. This results in an anthropogenic
                      radiative forcing associated with mineral dust
                      notwithstanding the natural origin of most aeolian dust.
                      Using the atmospheric chemistry climate model EMAC with a
                      detailed parametrisation of ageing processes and an emission
                      scheme accounting for the chemical composition of desert
                      soils, we study the direct radiative forcing globally and
                      regionally. Our results indicate large positive and negative
                      forcings, depending on the region. The predominantly
                      negative forcing at the top of the atmosphere over large
                      parts of the dust belt, from West Africa to East Asia,
                      attains a maximum of about −2W/m2 south of the Sahel, in
                      contrast to a positive forcing over India. Globally
                      averaged, these forcings partially counterbalance, resulting
                      in a net negative forcing of −0.05W/m2, which nevertheless
                      represents a considerable fraction of the total dust
                      forcing.},
      cin          = {IEK-8},
      ddc          = {550},
      cid          = {I:(DE-Juel1)IEK-8-20101013},
      pnm          = {243 - Tropospheric trace substances and their
                      transformation processes (POF3-243)},
      pid          = {G:(DE-HGF)POF3-243},
      typ          = {PUB:(DE-HGF)16},
      doi          = {10.5194/acp-2018-1104},
      url          = {https://juser.fz-juelich.de/record/858148},
}