Articles | Volume 20, issue 14
https://doi.org/10.5194/acp-20-8855-2020
© Author(s) 2020. 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-20-8855-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Cloudy-sky contributions to the direct aerosol effect
CICERO Center for International Climate Research, Oslo, Norway
Bjørn H. Samset
CICERO Center for International Climate Research, Oslo, Norway
Christian W. Mohr
CICERO Center for International Climate Research, Oslo, Norway
Kari Alterskjær
CICERO Center for International Climate Research, Oslo, Norway
Yves Balkanski
Laboratoire des Sciences du Climat et de l'Environnement,
CEA-CNRS-UVSQ-UPSaclay, Gif-sur-Yvette, France
Nicolas Bellouin
Department of Meteorology, University of Reading, Reading, RG6 6BB,
UK
Mian Chin
NASA Goddard Space Flight Center, Greenbelt, MD 20771, USA
James Haywood
College of Engineering, Mathematics and Physical Sciences, University
of Exeter, Exeter, EX4 4QF, UK
Earth System and Mitigation Science, Met Office Hadley Centre, Exeter, EX1 3PB, UK
Øivind Hodnebrog
CICERO Center for International Climate Research, Oslo, Norway
Stefan Kinne
Max Planck Institute for Meteorology, Hamburg, Germany
Guangxing Lin
Department of Climate and Space Sciences and Engineering, University
of Michigan, Ann Arbor, MI 48109, USA
now at: Atmospheric Sciences & Global Change Division, Pacific
Northwest National Laboratory, Richland, WA 99352, USA
Marianne T. Lund
CICERO Center for International Climate Research, Oslo, Norway
Joyce E. Penner
Department of Climate and Space Sciences and Engineering, University
of Michigan, Ann Arbor, MI 48109, USA
Michael Schulz
Norwegian Meteorological Institute, Oslo, Norway
Nick Schutgens
Earth Sciences, Faculty of Science, Vrije Universiteit Amsterdam,
Amsterdam, the Netherlands
Ragnhild B. Skeie
CICERO Center for International Climate Research, Oslo, Norway
Philip Stier
Atmospheric, Oceanic and Planetary Physics, Department of Physics,
University of Oxford, Oxford, UK
Toshihiko Takemura
Research Institute for Applied Mechanics, Kyushu University, Fukuoka,
Japan
Kai Zhang
Pacific Northwest National Laboratory, Richland, WA 99352, USA
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8 citations as recorded by crossref.
- Future evolution of aerosols and implications for climate change in the Euro-Mediterranean region using the CNRM-ALADIN63 regional climate model T. Drugé et al. 10.5194/acp-21-7639-2021
- Sensitivity of global direct aerosol shortwave radiative forcing to uncertainties in aerosol optical properties J. Elsey et al. 10.5194/acp-24-4065-2024
- Distributions and Trends of the Aerosol Direct Radiative Effect in the 21st Century: Aerosol and Environmental Contributions Q. Yu & Y. Huang 10.1029/2022JD037716
- Photoacoustic studies of energy transfer from ozone photoproducts to bath gases following Chappuis band photoexcitation M. Cotterell et al. 10.1039/D0CP05056C
- Scattering and absorbing aerosols in the climate system J. Li et al. 10.1038/s43017-022-00296-7
- A seven-year-based characterization of aerosol light scattering properties at a rural central European site L. Suchánková et al. 10.1016/j.atmosenv.2023.120292
- Size-resolved dust direct radiative effect efficiency derived from satellite observations Q. Song et al. 10.5194/acp-22-13115-2022
- On the differences in the vertical distribution of modeled aerosol optical depth over the southeastern Atlantic I. Chang et al. 10.5194/acp-23-4283-2023
1 citations as recorded by crossref.
Latest update: 20 Nov 2024
Short summary
The radiative forcing of the direct aerosol effects can be decomposed into clear-sky and cloudy-sky portions. In this study we use observational methods and two sets of multi-model global aerosol simulations over the industrial era to show that the contribution from cloudy-sky regions is likely weak.
The radiative forcing of the direct aerosol effects can be decomposed into clear-sky and...
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