The role of low-volatility organic compounds in initial particle growth in the atmosphere.
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Atmospheric science: Unexpected player in particle formation.Reduced anthropogenic aerosol radiative forcing caused by biogenic new particle formation.Global distribution of particle phase state in atmospheric secondary organic aerosolsAtmospheric gas-to-particle conversion: why NPF events are observed in megacities?Spiers Memorial Lecture. Introductory lecture: chemistry in the urban atmosphere.Highlights from Faraday Discussion: Chemistry in the urban atmosphere, United Kingdom, April 2016.Environmental conditions regulate the impact of plants on cloud formation.Solar eclipse demonstrating the importance of photochemistry in new particle formation.Reactive oxygen species formed in aqueous mixtures of secondary organic aerosols and mineral dust influencing cloud chemistry and public health in the Anthropocene.Microlayer source of oxygenated volatile organic compounds in the summertime marine Arctic boundary layer.Particle formation and growth from oxalic acid, methanesulfonic acid, trimethylamine and water: a combined experimental and theoretical study.Detection and identification of Criegee intermediates from the ozonolysis of biogenic and anthropogenic VOCs: comparison between experimental measurements and theoretical calculations.The effect of sub-zero temperature on the formation and composition of secondary organic aerosol from ozonolysis of alpha-pinene.Novel insights on new particle formation derived from a pan-european observing system.Impact on short-lived climate forcers increases projected warming due to deforestation.Perspective: Aerosol microphysics: From molecules to the chemical physics of aerosols.Terpene Composition Complexity Controls Secondary Organic Aerosol Yields from Scots Pine Volatile Emissions.Impact on short-lived climate forcers (SLCFs) from a realistic land-use change scenario via changes in biogenic emissions.Observations of biogenic ion-induced cluster formation in the atmosphere.Photo-tautomerization of acetaldehyde as a photochemical source of formic acid in the troposphere.Causes and importance of new particle formation in the present-day and preindustrial atmospheresCosmic rays, aerosols, clouds, and climate: Recent findings from the CLOUD experimentInfluence of temperature on the molecular composition of ions and charged clusters during pure biogenic nucleationSynergistic O + OH oxidation pathway to extremely low-volatility dimers revealed in β-pinene secondary organic aerosolNitrate radicals and biogenic volatile organic compounds: oxidation, mechanisms, and organic aerosolUnimolecular reaction of acetone oxide and its reaction with water in the atmosphereReal-time detection of highly oxidized organosulfates and BSOA marker compounds during the F-BEACh 2014 field studyChemical characterization of atmospheric ions at the high altitude research station Jungfraujoch (Switzerland)Simultaneous measurements of new particle formation at 1 s time resolution at a street site and a rooftop siteModeling the role of highly oxidized multifunctional organic molecules for the growth of new particles over the boreal forest regionTechnical note: Relating functional group measurements to carbon types for improved model–measurement comparisons of organic aerosol compositionDynamic consideration of smog chamber experimentsMATRIX-VBS (v1.0): implementing an evolving organic aerosol volatility in an aerosol microphysics modelIsoprene suppression of new particle formation: Potential mechanisms and implicationsWall effects in smog chamber experiments: A model studyImportant global and regional differences in aerosol cloud-albedo effect estimates between simulations with and without prognostic aerosol microphysicsRapid growth of organic aerosol nanoparticles over a wide tropospheric temperature rangeRobust metric for quantifying the importance of stochastic effects on nanoparticle growthQuantitation of 11 alkylamines in atmospheric samples: separating structural isomers by ion chromatographyCloud-seeding surprise could improve climate predictions
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P2860
The role of low-volatility organic compounds in initial particle growth in the atmosphere.
description
2016 nî lūn-bûn
@nan
2016年の論文
@ja
2016年論文
@yue
2016年論文
@zh-hant
2016年論文
@zh-hk
2016年論文
@zh-mo
2016年論文
@zh-tw
2016年论文
@wuu
2016年论文
@zh
2016年论文
@zh-cn
name
The role of low-volatility org ...... icle growth in the atmosphere.
@en
The role of low-volatility org ...... icle growth in the atmosphere.
@nl
type
label
The role of low-volatility org ...... icle growth in the atmosphere.
@en
The role of low-volatility org ...... icle growth in the atmosphere.
@nl
prefLabel
The role of low-volatility org ...... icle growth in the atmosphere.
@en
The role of low-volatility org ...... icle growth in the atmosphere.
@nl
P2093
P50
P356
P1154
2-s2.0-84971350459
P1433
P1476
The role of low-volatility organic compounds in initial particle growth in the atmosphere
@en
P2093
Alessandro Franchin
Alexey Adamov
Andrea C Wagner
Antti Onnela
Antònio Dias
Ari Laaksonen
Carla Frege
Christina Williamson
Claudia Fuchs
P2888
P304
P356
10.1038/NATURE18271
P407
P50
P5530
P577
2016-05-01T00:00:00Z
P6179
1012369807