Reduced anthropogenic aerosol radiative forcing caused by biogenic new particle formation

550 aerosol FORMATION EVENTS IMPACT Climate 551 History, 18th Century 01 natural sciences SULFURIC-ACID ATMOSPHERIC PARTICLES BIOGENIC SDG 13 - Climate Action Industrial Development EMISSIONS Air Pollutants [SPI.FLUID]Engineering Sciences [physics]/Reactive fluid environment Uncertainty AEROSOL History, 19th Century FOREST SDG 13 – Maßnahmen zum Klimaschutz SDG 9 - Industry NUCLEATION 103039 Aerosol physics History, 21st Century [SPI.AUTO]Engineering Sciences [physics]/Automatic forcing SECONDARY ORGANIC AEROSOL GLOBAL CCN Humans Computer Simulation 103039 Aerosolphysik Innovation climate Aerosol 0105 earth and related environmental sciences Aerosols Models, Statistical Atmosphere FORCING CLIMATE MODEL History, 20th Century CLIMATE 13. Climate action 103037 Environmental physics and Infrastructure Biogenic Forcing biogenic 103037 Umweltphysik
DOI: 10.1073/pnas.1602360113 Publication Date: 2016-10-11T17:24:07Z
ABSTRACT
Significance A mechanism for the formation of atmospheric aerosols via the gas to particle conversion of highly oxidized organic molecules is found to be the dominant aerosol formation process in the preindustrial boundary layer over land. The inclusion of this process in a global aerosol model raises baseline preindustrial aerosol concentrations and could lead to a reduction of 27% in estimates of anthropogenic aerosol radiative forcing.
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