@Article{FanRZGLMMYWABBCFGGMPPPS:2018:SuCoPr,
author = "Fan, Jiwen and Rosenfeld, Daniel and Zhang, Yuwei and Giangrande,
Scott E. and Li, Zhanqing and Machado, Luiz Augusto Toledo and
Martin, Scot T. and Yang, Yan and Wang, Jian and Artaxo, Paulo and
Barbosa, Henrique M. J. and Braga, Ramon Campos and Comstock,
Jennifer M. and Feng, Zhe and Gao, Wenhua and Gomes, Helber B. and
Mei, Fan and P{\"o}hlker, Christopher and P{\"o}hlker, Mira L.
and P{\"o}schl, Ulrich and Souza, Rodrigo A. F. de",
affiliation = "{Pacific Northwest National Laboratory} and {Hebrew University of
Jerusalem} and {Pacific Northwest National Laboratory} and
{Brookhaven National Laboratory} and {University of Maryland} and
{Instituto Nacional de Pesquisas Espaciais (INPE)} and {Harvard
University} and {Pacific Northwest National Laboratory} and
{Brookhaven National Laboratory} and {Universidade de S{\~a}o
Paulo (USP)} and {Universidade de S{\~a}o Paulo (USP)} and
{Instituto Nacional de Pesquisas Espaciais (INPE)} and {Pacific
Northwest National Laboratory} and {Pacific Northwest National
Laboratory} and {Pacific Northwest National Laboratory} and
{Univerisdade Federal de Alagoas (UFAL)} and {Pacific Northwest
National Laboratory} and {Max Planck Institute for Chemistry} and
{Max Planck Institute for Chemistry} and {Max Planck Institute for
Chemistry} and {Universidade do Estado do Amazonas (UEA)}",
title = "Substantial convection and precipitation enhancements by ultrafine
aerosol particles",
journal = "Science",
year = "2018",
volume = "359",
number = "6374",
pages = "411--418",
month = "jan.",
abstract = "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.
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.",
doi = "10.1126/science.aan8461",
url = "http://dx.doi.org/10.1126/science.aan8461",
issn = "0036-8075",
language = "en",
targetfile = "fan_substantial.pdf",
urlaccessdate = "19 abr. 2024"
}