Anthropogenic emissions and land use changes have modified atmospheric aerosol
concentrations and size distributions over time. Understanding preindustrial conditions and …

Secondary organic aerosol (SOA) is formed in the atmosphere when volatile organic
compounds (VOCs) emitted from anthropogenic and biogenic sources are oxidized by …

Oxidation of biogenic volatile organic compounds (BVOC) by the nitrate radical (NO 3)
represents one of the important interactions between anthropogenic emissions related to …

Secondary organic aerosol (SOA) accounts for a significant fraction of ambient tropospheric
aerosol and a detailed knowledge of the formation, properties and transformation of SOA is …

This report is the first complete assessment of the science of climate change since Working
Group I (WGI) of the IPCC produced its second report Climate Change 1995: The Science of …

This paper evaluates the current status of global modeling of the organic aerosol (OA) in the
troposphere and analyzes the differences between models as well as between models and …

We discuss the use of a two-dimensional volatility-oxidation space (2-D-VBS) to describe
organic-aerosol chemical evolution. The space is built around two coordinates, volatility and …

This article describes the governing equations, computational algorithms, and other
components entering into the Community Multiscale Air Quality (CMAQ) modeling system …

Atmospheric aerosol particles serve as condensation nuclei for the formation of both, cloud
droplets and atmospheric ice particles. As a result, they exert a substantial influence on the …

Secondary organic aerosol (SOA), particulate matter composed of compounds formed from
the atmospheric transformation of organic species, accounts for a substantial fraction of …