Articles | Volume 17, issue 19
https://doi.org/10.5194/acp-17-12145-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/acp-17-12145-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Uncertainty from the choice of microphysics scheme in convection-permitting models significantly exceeds aerosol effects
Bethan White
CORRESPONDING AUTHOR
Atmospheric, Oceanic and Planetary Physics, University of Oxford, Oxford, UK
Edward Gryspeerdt
Institute for Meteorology, Universität Leipzig, Leipzig, Germany
Philip Stier
Atmospheric, Oceanic and Planetary Physics, University of Oxford, Oxford, UK
Hugh Morrison
National Center for Atmospheric Research, Boulder, Colorado, USA
Gregory Thompson
National Center for Atmospheric Research, Boulder, Colorado, USA
Zak Kipling
European Centre for Medium-Range Weather Forecasts, Shinfield Park, Reading, UK
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44 citations as recorded by crossref.
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- Atmospheric energy budget response to idealized aerosol perturbation in tropical cloud systems G. Dagan et al. 10.5194/acp-20-4523-2020
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- Tropical and Boreal Forest – Atmosphere Interactions: A Review P. Artaxo et al. 10.16993/tellusb.34
- Seamless Modeling of Direct and Indirect Aerosol Effects during April 2020 Wildfire Episode in Ukraine M. Savenets et al. 10.3390/atmos15050550
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- Comparisons of bin and bulk microphysics schemes in simulations of topographic winter precipitation with radar and radiometer measurements M. Han et al. 10.1002/qj.3393
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Discussed (preprint)
Latest update: 20 Nov 2024
Short summary
Aerosols influence cloud and precipitation by modifying cloud droplet number concentrations (CDNCs). We simulate three different types of convective cloud using two different cloud microphysics parameterisations. The simulated cloud and precipitation depends much more strongly on the choice of microphysics scheme than on CDNC. The uncertainty differs between types of convection. Our results highlight a large uncertainty in cloud and precipitation responses to aerosol in current models.
Aerosols influence cloud and precipitation by modifying cloud droplet number concentrations...
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