Articles | Volume 19, issue 7
https://doi.org/10.5194/acp-19-4763-2019
© Author(s) 2019. 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-19-4763-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
BVOC–aerosol–climate feedbacks investigated using NorESM
Department of Geosciences, University of Oslo, Oslo, Norway
Sara M. Blichner
Department of Geosciences, University of Oslo, Oslo, Norway
Inger H. H. Karset
Department of Geosciences, University of Oslo, Oslo, Norway
Risto Makkonen
Climate System Research, Finnish Meteorological Institute, P.O. Box
503, Helsinki, Finland
Institute for Atmospheric and Earth
System Research/Physics, Faculty of Science, P.O. Box 64, 00014, University
of Helsinki, Helsinki, Finland
Terje K. Berntsen
Department of Geosciences, University of Oslo, Oslo, Norway
CICERO Center for International
Climate Research, Oslo, Norway
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Latest update: 14 Dec 2024
Short summary
In this study, an Earth system model has been used to investigate climate feedbacks associated with increasing BVOC emissions due to higher CO2 concentrations and temperatures. Higher BVOC emissions associated with a changed climate are found to induce an important negative climate feedback through increased aerosol formation and resulting changes in cloud properties. This feedback is found to have the potential to offset about 13 % of the radiative forcing associated with a doubling of CO2.
In this study, an Earth system model has been used to investigate climate feedbacks associated...
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