The DOI matches its Crossref record; 62 of the 66 references it cites were found in a registry or an index.
Weak average liquid-cloud-water response to anthropogenic aerosols
Open accessAbstract
The cooling of the Earth's climate through the effects of anthropogenic aerosols on clouds offsets an unknown fraction of greenhouse gas warming. An increase in the amount of water inside liquid-phase clouds induced by aerosols, through the suppression of rain formation, has been postulated to lead to substantial cooling, which would imply that the Earth's surface temperature is highly sensitive to anthropogenic forcing. Here we provide direct observational evidence that, instead of a strong increase, aerosols cause a relatively weak average decrease in the amount of water in liquid-phase clouds compared with unpolluted clouds. Measurements of polluted clouds downwind of various anthropogenic sources-such as oil refineries, smelters, coal-fired power plants, cities, wildfires and ships-reveal that aerosol-induced cloud-water increases, caused by suppressed rain formation, and decreases, caused by enhanced evaporation of cloud water, partially cancel each other out. We estimate that the observed decrease in cloud water offsets 23% of the global climate-cooling effect caused by aerosol-induced increases in the concentration of cloud droplets. These findings invalidate the hypothesis that increases in cloud water cause a substantial climate cooling effect and translate into reduced uncertainty in projections of future climate.
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“More recent studies show that aerosols can also change LWP and total cloud fraction (CF), which also greatly affect the amount of solar radiation reflected by clouds2,13–16.”
From Abrupt reduction in shipping emission as an inadvertent geoengineering termination shock produces substantial radiative warming (2024) · cites this paper as [16]
Citations
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Cited by
Sorted by citations
Bounding Global Aerosol Radiative Forcing of Climate Change
Bellouin, N., Quaas, J., Gryspeerdt, E., Kinne, S., Stier, P., Watson‐Parris, D., Boucher, O., Carslaw, K. S., Christensen, M., Daniau, A. ‐., et al. (2020) · Reviews of Geophysics · doi:10.1029/2019rg000660 · Cited by 1,116
“…although possible in individual1168 clouds, are unlikely to hold on average according to the analyses of ship, volcano, and1169 pollution tracks by Toll et al. (2017, 2019).1170 8.2 Adjustments in cloud cover C1171 The suppression of precipitation may also lead to a change in C, either via…”
BackgroundInfluentialSelf-citationScattering and absorbing aerosols in the climate system
Li, J., Carlson, B. E., Yung, Y. L., Lv, D., Hansen, J. E., Penner, J. E., Liao, H., Ramaswamy, V., Kahn, R. A., Zhang, P., et al. (2022) · Nature Reviews Earth & Environment · doi:10.1038/s43017-022-00296-7 · Cited by 677
“…et al., 2018 Mulcahy et al., 2018 Petersik et al., 2018 Rémy et al., 2018 Zhou et al., 2018 Hasekamp et al., 2019 Kinne, 2019 Matus et al., 2019 Toll et al., 2019 Yoshioka et al., 2019 Bellouin et al., 2020 Diamond et al., 2020 Dittus et al., 2020 Douglas & Ecuyer, 2020 Gryspeert et al.,…”
BackgroundAerosols enhance cloud lifetime and brightness along the stratus-to-cumulus transition
Christensen, M. W., Jones, W. K., & Stier, P. (2020) · Proceedings of the National Academy of Sciences · doi:10.1073/pnas.1921231117 · Cited by 265
Self-citationAerosol-cloud-climate cooling overestimated by ship-track data
Glassmeier, F., Hoffmann, F., Johnson, J. S., Yamaguchi, T., Carslaw, K. S., & Feingold, G. (2021) · Science · doi:10.1126/science.abd3980 · Cited by 205
“Numerical values for LWP-adjustments dlnLWP/dlnN have been derived from detailed modeling and satellite studies [20, 8, 21, 22, 23, 14, 15, 24, 25, 16, 17].”
BackgroundMethodResultInfluentialAerosol‐Forced AMOC Changes in CMIP6 Historical Simulations
Menary, M. B., Robson, J. I., Allan, R. P., Booth, B. B. B., Cassou, C., Gastineau, G., Gregory, J. M., Hodson, D., Jones, C., Mignot, J., et al. (2020) · Geophysical Research Letters · doi:10.1029/2020gl088166 · Cited by 186
“, 2013), and recent observational and cloud‐resolving modeling studies have also suggested that the indirect aerosol effect might have been overestimated in many climate models (Sato et al., 2018; Toll et al., 2019).”
Background
Metadata
- Authors
- Toll, V., Christensen, M., Quaas, J., & Bellouin, N.
- Affiliations
- University of Tartu (EE)
- University of Oxford (GB)
- Leipzig University (DE)
- University of Reading (GB)
- Corresponding author
- Toll, Velle
- Venue
- Nature
- Published
- 2019-07-31
- Volume
- 572
- Issue
- 7767
- Pages
- 51-55
- ISSN
- 0028-0836 (ISSN-L)
- 1476-4687
- OpenAlex
- W2965102826
- Cited by
- 254
- References
- 66
- Citations by year
- 2026: 17 · 2025: 32 · 2024: 40 · 2023: 45 · 2022: 42 · 2021: 41 · 2020: 31 · 2019: 6
- FWCI
- 15.44
- Type
- journal article
- Language
- en
- Update notices
- correction (2020-01-03)
- Open access
- Licence
- Locations
- Nature (publishedVersion)
- PubMed (publishedVersion)
- CentAUR (University of Reading) (acceptedVersion)
- RePEc: Research Papers in Economics (submittedVersion)
- Funders
- University of Reading
- Eesti Teadusagentuur (PSG202)
- Natural Environment Research Council (NE/L013746/1, NE/L013479/1)
- Topics
- Physical Sciences › Environmental Science › Global and Planetary Change › Atmospheric aerosols and clouds
- Physical Sciences › Earth and Planetary Sciences › Atmospheric Science › Atmospheric chemistry and aerosols
- Physical Sciences › Environmental Science › Global and Planetary Change › Climate Change and Geoengineering
- Keywords
- anthropogenic aerosols, cloud water content, aerosol-cloud interactions, cloud droplet number concentration, cloud evaporation, climate cooling effect, global warming, climate sensitivity
- MeSH terms
- Aerosols, Air Pollution, Human Activities, Models, Theoretical, Rain, Temperature, Water, Greenhouse Effect, Uncertainty, Climate Change
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