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Substantial convection and precipitation enhancements by ultrafineaerosol particles

Up with ultrafine aerosol particles Ultrafine aerosol particles (smaller than 50 nanometers in diameter) have beenthought to be too small to affect cloud formation. Fan et al.show that this is not the case. They studied the effect of urban pollutiontransported into the otherwise nearly pristine atmo... Full description

Journal Title: Science Jan 26, 2018, Vol.359(6374), pp.411-418
Main Author: Rosenfeld, Daniel
Other Authors: Zhang, Yuwei , Giangrande, Scott , Li, Zhanqing , Martin, Scot , Yang, Yan , Wang, Jian , Braga, Ramon , Comstock, Jennifer , Gomes, Helber , Fan, Mei , Pöhlker, Mira
Format: Electronic Article Electronic Article
Language: English
Subjects:
ID: ISSN: 00368075 ; E-ISSN: 10959203 ; DOI: 10.1126/science.aan8461
Link: http://search.proquest.com/docview/1993029187/?pq-origsite=primo
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title: Substantial convection and precipitation enhancements by ultrafineaerosol particles
format: Article
creator:
  • Rosenfeld, Daniel
  • Zhang, Yuwei
  • Giangrande, Scott
  • Li, Zhanqing
  • Martin, Scot
  • Yang, Yan
  • Wang, Jian
  • Braga, Ramon
  • Comstock, Jennifer
  • Gomes, Helber
  • Fan, Mei
  • Pöhlker, Mira
subjects:
  • Troposphere
  • Clouds
  • Atmospheric Convection
  • Supersaturation
  • Atmospheric Convection
  • Air Pollution
  • Clouds
  • Water Pollution
  • Airborne Particulates
  • Droplets
  • Computer Simulation
  • Coalescence
  • Clouds
  • Plumes
  • Rainfall
  • Surface Area
  • Troposphere
  • Plumes
  • Plumes
  • Particulates
ispartof: Science, Jan 26, 2018, Vol.359(6374), pp.411-418
description: Up with ultrafine aerosol particles Ultrafine aerosol particles (smaller than 50 nanometers in diameter) have beenthought to be too small to affect cloud formation. Fan et al.show that this is not the case. They studied the effect of urban pollutiontransported into the otherwise nearly pristine atmosphere of the Amazon.Condensational growth of water droplets around the tiny particles releaseslatent heat, thereby intensifying atmospheric convection. Thus, anthropogenicultrafine aerosol particles may exert a more important influence on cloudformation processes than previously believed. Science, this issue p. 411 Aerosol-cloud interactions remain the largest uncertainty in climate projections.Ultrafine aerosol particles smaller than 50 nanometers (UAP
language: eng
source:
identifier: ISSN: 00368075 ; E-ISSN: 10959203 ; DOI: 10.1126/science.aan8461
fulltext: no_fulltext
issn:
  • 00368075
  • 0036-8075
  • 10959203
  • 1095-9203
url: Link


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titleSubstantial convection and precipitation enhancements by ultrafineaerosol particles
creatorRosenfeld, Daniel ; Zhang, Yuwei ; Giangrande, Scott ; Li, Zhanqing ; Martin, Scot ; Yang, Yan ; Wang, Jian ; Braga, Ramon ; Comstock, Jennifer ; Gomes, Helber ; Fan, Mei ; Pöhlker, Mira
ispartofScience, Jan 26, 2018, Vol.359(6374), pp.411-418
identifier
subjectTroposphere ; Clouds ; Atmospheric Convection ; Supersaturation ; Atmospheric Convection ; Air Pollution ; Clouds ; Water Pollution ; Airborne Particulates ; Droplets ; Computer Simulation ; Coalescence ; Clouds ; Plumes ; Rainfall ; Surface Area ; Troposphere ; Plumes ; Plumes ; Particulates
descriptionUp with ultrafine aerosol particles Ultrafine aerosol particles (smaller than 50 nanometers in diameter) have beenthought to be too small to affect cloud formation. Fan et al.show that this is not the case. They studied the effect of urban pollutiontransported into the otherwise nearly pristine atmosphere of the Amazon.Condensational growth of water droplets around the tiny particles releaseslatent heat, thereby intensifying atmospheric convection. Thus, anthropogenicultrafine aerosol particles may exert a more important influence on cloudformation processes than previously believed. Science, this issue p. 411 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 smallto affect cloud formation. Observational evidence and numerical simulations ofdeep convective clouds (DCCs) over the Amazon show that DCCs forming in alow-aerosol...
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titleSubstantial convection and precipitation enhancements by ultrafineaerosol particles
descriptionUp with ultrafine aerosol particles Ultrafine aerosol particles (smaller than 50 nanometers in diameter) have beenthought to be too small to affect cloud formation. Fan et al.show that this is not the case. They studied the effect of urban pollutiontransported into the otherwise nearly pristine atmosphere of the Amazon.Condensational growth of water droplets around the tiny particles releaseslatent heat, thereby intensifying atmospheric convection. Thus, anthropogenicultrafine aerosol particles may exert a more important influence on cloudformation processes than previously believed. Science, this issue p. 411 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 smallto affect cloud formation. Observational evidence and numerical simulations ofdeep convective clouds (DCCs) over the Amazon show that DCCs forming in alow-aerosol...
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citationpf 411 pt 418 vol 359 issue 6374
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titleSubstantial convection and precipitation enhancements by ultrafineaerosol particles
authorRosenfeld, Daniel ; Zhang, Yuwei ; Giangrande, Scott ; Li, Zhanqing ; Martin, Scot ; Yang, Yan ; Wang, Jian ; Braga, Ramon ; Comstock, Jennifer ; Gomes, Helber ; Fan, Mei ; Pöhlker, Mira
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8Computer Simulation
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abstractUp with ultrafine aerosol particles Ultrafine aerosol particles (smaller than 50 nanometers in diameter) have beenthought to be too small to affect cloud formation. Fan et al.show that this is not the case. They studied the effect of urban pollutiontransported into the otherwise nearly pristine atmosphere of the Amazon.Condensational growth of water droplets around the tiny particles releaseslatent heat, thereby intensifying atmospheric convection. Thus, anthropogenicultrafine aerosol particles may exert a more important influence on cloudformation processes than previously believed. Science, this issue p. 411 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 smallto affect cloud formation. Observational evidence and numerical simulations ofdeep convective clouds (DCCs) over the Amazon show that DCCs forming in alow-aerosol...
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pubThe American Association for the Advancement of Science
doi10.1126/science.aan8461
urlhttp://search.proquest.com/docview/1993029187/
orcidid0000000152804391
date2018-01-26