Substantial convection and precipitation enhancements by ultrafine aerosol particles
- Pacific Northwest National Lab. (PNNL), Richland, WA (United States). Atmospheric Science and Global Change Div. (ASGC)
- Hebrew Univ. of Jerusalem (Israel). Inst. of Earth Sciences
- Pacific Northwest National Lab. (PNNL), Richland, WA (United States). Atmospheric Science and Global Change Div. (ASGC); Univ. of Maryland, College Park, MD (United States). Dept. of Atmospheric and Oceanic Science and ESSIC
- Brookhaven National Lab. (BNL), Upton, NY (United States). Environmental and Climate Science Dept.
- Univ. of Maryland, College Park, MD (United States). Dept. of Atmospheric and Oceanic Science and ESSIC; Beijing Normal Univ., Beijing (China). State Lab. of Earth Surface Process and Resource Ecology, GCESS
- National Inst. for Space Research, Cachoeira Paulista (Brazil). Weather Prevision Center and Climate Studies
- Harvard Univ., Cambridge, MA (United States). School of Engineering and Applied Sciences (SEAS)
- Pacific Northwest National Lab. (PNNL), Richland, WA (United States). Atmospheric Science and Global Change Div. (ASGC); Beijing Municipal Weather Modification Office, Beijing (China)
- Univ. of Sao Paulo (Brazil). Inst. of Physics
- Univ. of Sao Paulo (Brazil). Inst. of Physics; Univ. of Maryland Baltimore County (UMBC), Baltimore, MD (United States). Dept. of Physics
- Pacific Northwest National Lab. (PNNL), Richland, WA (United States). Atmospheric Science and Global Change Div. (ASGC); Chinese Academy of Meteorological Sciences, Beijing (China). State Key Lab. of Severe Weather
- Federal Univ. of Alagoas (Brazil). Atmospheric and Climate Dynamics Lab. and Inst. of Atmospheric Sciences
- Max Planck Society, Mainz (Germany). Max Planck Inst. for Chemistry and Multiphase Chemistry and Biogeochemistry Dept.
- Max Planck Society, Mainz (Germany). Max Planck Inst. for Chemistry and Multiphase Chemistry and Biogeochemistry Dept.; Johannes Gutenberg Univ., Mainz (Germany)
- Amazonas State Univ. (UEA), Manaus-AM (Brazil). School of Technology and Dept. of Meteorology
Aerosol-cloud interactions remain the largest uncertainty in climate projections. Ultrafine aerosol particles smaller than 50 nanometers (UAP<50) can be abundant in the troposphere, but are conventionally considered too small to affect cloud formation. However, observational evidence and numerical simulations of deep convective clouds (DCCs) over the Amazon show that DCCs forming in a low aerosol environment can develop very large vapor supersaturation because fast droplet coalescence reduces integrated droplet surface area and subsequent condensation. UAP<50 from pollution plumes that are ingested into such clouds can be activated to form additional cloud droplets on which excess supersaturation condenses and forms additional cloud water and latent heating, thus intensifying convective strength. This mechanism suggests a strong anthropogenic invigoration of DCCs in previously pristine regions of the world.
- Research Organization:
- Brookhaven National Laboratory (BNL), Upton, NY (United States)
- Sponsoring Organization:
- USDOE Office of Science (SC), Biological and Environmental Research (BER) (SC-23); National Science Foundation (NSF), Washington, DC (United States); National Science Foundation of China; European Union (EU); Cloud Processes of the Main Precipitation System (CHUVA) project; National Institute of Amazonian Research (INPA); Amazonas State Univ. (UEA); Amazonas State Research Support Foundation (FAPEAM); National Council for Scientific and Technological Development (CNPq); German Federal Ministry of Education and Research (BMBF)
- Grant/Contract Number:
- SC0012704; AC06-76RL01830
- OSTI ID:
- 1424983
- Alternate ID(s):
- OSTI ID: 1427899; OSTI ID: 1438524
- Report Number(s):
- BNL-203206-2018-JAAM
- Journal Information:
- Science, Journal Name: Science Journal Issue: 6374 Vol. 359; ISSN 0036-8075
- Publisher:
- AAASCopyright Statement
- Country of Publication:
- United States
- Language:
- English
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