Articles | Volume 15, issue 13
https://doi.org/10.5194/acp-15-7557-2015
© Author(s) 2015. 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-15-7557-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Research article
| 
13 Jul 2015
Research article |
| 13 Jul 2015
Wet scavenging limits the detection of aerosol effects on precipitation
E. Gryspeerdt
CORRESPONDING AUTHOR
Department of Physics, University of Oxford, Oxford, UK
Institute for Meteorology, Universität Leipzig, Leipzig, Germany
Department of Physics, University of Oxford, Oxford, UK
B. A. White
Department of Physics, University of Oxford, Oxford, UK
Z. Kipling
Department of Physics, University of Oxford, Oxford, UK
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- A study of the impact of synoptic weather conditions and water vapor on aerosol–cloud relationships over major urban clusters of China K. Kourtidis et al. 10.5194/acp-15-10955-2015
- Rain‐aerosol relationships influenced by wind speed Y. Yang et al. 10.1002/2016GL067770
- Opinion: A critical evaluation of the evidence for aerosol invigoration of deep convection A. Varble et al. 10.5194/acp-23-13791-2023
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- Addressing the difficulties in quantifying droplet number response to aerosol from satellite observations H. Jia et al. 10.5194/acp-22-7353-2022
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- Unveiling aerosol–cloud interactions – Part 2: Minimising the effects of aerosol swelling and wet scavenging in ECHAM6-HAM2 for comparison to satellite data D. Neubauer et al. 10.5194/acp-17-13165-2017
- An Unknown Maximum Lag‐Correlation Between Rainfall and Aerosols at 140–160 Minutes P. Alpert et al. 10.1029/2020GL089334
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- Tropical and Boreal Forest – Atmosphere Interactions: A Review P. Artaxo et al. 10.16993/tellusb.34
- Passive remote sensing of aerosol layer height using near‐UV multiangle polarization measurements L. Wu et al. 10.1002/2016GL069848
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1 citations as recorded by crossref.
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Latest update: 15 Nov 2024
Short summary
Wet scavenging generates differences between the aerosol properties in clear-sky scenes (observed by satellites) and cloudy scenes, leading to different
aerosol-precipitation relationships in satellite data and global models. Convective systems usually draw in air from clear-sky regions, but global models have difficulty separating this aerosol from the aerosol in cloudy scenes within a model gridbox. This may prevent models from reproducing the observed aerosol-precipitation relationships.
Wet scavenging generates differences between the aerosol properties in clear-sky scenes...
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