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@ARTICLE{Klingmller:891837,
      author       = {Klingmüller, Klaus and Karydis, Vlassis A. and Bacer, Sara
                      and Stenchikov, Georgiy L. and Lelieveld, Jos},
      title        = {{W}eaker cooling by aerosols due to dust–pollution
                      interactions},
      journal      = {Atmospheric chemistry and physics},
      volume       = {20},
      number       = {23},
      issn         = {1680-7324},
      address      = {Katlenburg-Lindau},
      publisher    = {EGU},
      reportid     = {FZJ-2021-01760},
      pages        = {15285 - 15295},
      year         = {2020},
      abstract     = {The interactions between aeolian dust and anthropogenic air
                      pollution, notably chemical ageing of mineral dust and
                      coagulation of dust and pollution particles, modify the
                      atmospheric aerosol composition and burden. Since the
                      aerosol particles can act as cloud condensation nuclei, this
                      affects the radiative transfer not only directly via
                      aerosol–radiation interactions, but also indirectly
                      through cloud adjustments. We study both radiative effects
                      using the global ECHAM/MESSy atmospheric chemistry-climate
                      model (EMAC) which combines the Modular Earth Submodel
                      System (MESSy) with the European Centre/Hamburg (ECHAM)
                      climate model. Our simulations show that
                      dust–pollution–cloud interactions reduce the condensed
                      water path and hence the reflection of solar radiation. The
                      associated climate warming outweighs the cooling that the
                      dust–pollution interactions exert through the direct
                      radiative effect. In total, this results in a net warming by
                      dust–pollution interactions which moderates the negative
                      global anthropogenic aerosol forcing at the top of the
                      atmosphere by (0.2 ± 0.1) W m−2.},
      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},
      UT           = {WOS:000599336000001},
      doi          = {10.5194/acp-20-15285-2020},
      url          = {https://juser.fz-juelich.de/record/891837},
}