Articles | Volume 21, issue 1
https://doi.org/10.5194/acp-21-17-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/acp-21-17-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Cloud adjustments dominate the overall negative aerosol radiative effects of biomass burning aerosols in UKESM1 climate model simulations over the south-eastern Atlantic
Atmospheric, Oceanic and Planetary Physics, Department of Physics,
University of Oxford, Oxford, OX1 3PU, UK
now at: Department of Geophysics, Tel Aviv University, Tel Aviv 69978, Israel
Philip Stier
Atmospheric, Oceanic and Planetary Physics, Department of Physics,
University of Oxford, Oxford, OX1 3PU, UK
Hamish Gordon
School of Earth and Environment, University of Leeds, Leeds, LS2 9JT, UK
now at: Engineering Research Accelerator, Carnegie Mellon University,
Pittsburgh, PA 15217, USA
Duncan Watson-Parris
Atmospheric, Oceanic and Planetary Physics, Department of Physics,
University of Oxford, Oxford, OX1 3PU, UK
Lucia Deaconu
Atmospheric, Oceanic and Planetary Physics, Department of Physics,
University of Oxford, Oxford, OX1 3PU, UK
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Latest update: 08 Dec 2024
Short summary
The south-eastern Atlantic is semi-permanently covered by some of the largest stratocumulus clouds and is influenced by one-third of the biomass burning emissions from African fires. A UKEMS1 model simulation shows that the absorption effect of biomass burning aerosols is the most significant on clouds and radiation. The dominate cooling and rapid adjustments induced by the radiative effects of biomass burning aerosols result in an overall cooling in the south-eastern Atlantic.
The south-eastern Atlantic is semi-permanently covered by some of the largest stratocumulus...
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