Articles | Volume 22, issue 3
https://doi.org/10.5194/acp-22-2095-2022
© Author(s) 2022. 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-22-2095-2022
© Author(s) 2022. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
15 Feb 2022
Research article |
| 15 Feb 2022
| 15 Feb 2022
How well do the CMIP6 models simulate dust aerosols?
Department of Meteorology, University of Reading, Reading, UK
National Centre for Atmospheric Science, Reading, UK
Claire L. Ryder
Department of Meteorology, University of Reading, Reading, UK
Laura J. Wilcox
Department of Meteorology, University of Reading, Reading, UK
National Centre for Atmospheric Science, Reading, UK
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- The Extreme North African Haboob in October 2008: High‐Resolution Simulation of Organized Moist Convection in the Lee of the Atlas, Dust Recirculation and Poleward Transport S. Dhital et al. 10.1029/2021JD035858
- Aerosol characteristics in CMIP6 models' global simulations and their evaluation with the satellite measurements J. Bharath et al. 10.1002/joc.8324
- Modelling the 2021 East Asia super dust storm using FLEXPART and FLEXDUST and its comparison with reanalyses and observations H. Tang et al. 10.3389/fenvs.2022.1013875
- Mineral dust aerosol impacts on global climate and climate change J. Kok et al. 10.1038/s43017-022-00379-5
- Elemental ratios as tracers of the sources of mineral dust in north-eastern Sahara M. Boraiy et al. 10.1007/s13762-023-05077-3
1 citations as recorded by crossref.
Latest update: 13 Dec 2024
Short summary
The CMIP6 models' simulated dust processes are getting more uncertain as models become more sophisticated. Of particular challenge are the links between dust cycles and optical properties, and we recommend more detailed output relating to dust cycles in future intercomparison projects to constrain such links. Also, models struggle to capture certain key regional dust processes such as dust accumulation along the slope of the Himalayas and dust seasonal cycles in North China and North America.
The CMIP6 models' simulated dust processes are getting more uncertain as models become more...
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