Javascript must be enabled to continue!
Assessment of biogenic secondary organic aerosol in the Himalayas
View through CrossRef
Environmental context
Secondary organic aerosols derived from biogenic gases are ubiquitous in the atmosphere. We found that biogenic secondary organic aerosol in Nepal accounted for 6 to 23 % of organic carbon. Primary and secondary biogenic sources combined accounted for approximately half of the observed organic aerosol, suggesting that additional aerosol sources or precursors are significant in this region of the Himalayas.
Abstract
Biogenic contributions to secondary organic aerosol (SOA) in the South-East Asian regional haze were assessed by measurement of isoprene, monoterpene and sesquiterpene photooxidation products in fine particles (PM2.5) at a mid-latitude site in the Himalayas. Organic species were measured in solvent extracts of filter samples using gas chromatography–mass spectrometry (GCMS) and chemical derivatisation; this analysis was used to quantify molecular markers for primary aerosol sources – including motor vehicles, biomass burning and detritus – and SOA tracers. Authentic standards of most SOA products were not commercially available at the time of this study, so surrogate standards were used for semiquantitation. Using an empirical approach to uncertainty estimation based on homologous series of atmospherically relevant model compounds, analytical uncertainties ranged from 32 % for SOA tracers with structurally similar surrogates to more than 100 % for tracers with a poorly matched surrogate. Biogenic SOA contributions to PM2.5 organic carbon content in the 2005 monsoon and post-monsoon season ranged from 2–19 % for isoprene, 1–5 % for monoterpenes and 1–4 % for sesquiterpenes. High concentrations of isoprene derivatives in aerosol, particularly in the late summer months, point to biogenic SOA as a significant source of organic carbon in the Himalayan region.
Title: Assessment of biogenic secondary organic aerosol in the Himalayas
Description:
Environmental context
Secondary organic aerosols derived from biogenic gases are ubiquitous in the atmosphere.
We found that biogenic secondary organic aerosol in Nepal accounted for 6 to 23 % of organic carbon.
Primary and secondary biogenic sources combined accounted for approximately half of the observed organic aerosol, suggesting that additional aerosol sources or precursors are significant in this region of the Himalayas.
Abstract
Biogenic contributions to secondary organic aerosol (SOA) in the South-East Asian regional haze were assessed by measurement of isoprene, monoterpene and sesquiterpene photooxidation products in fine particles (PM2.
5) at a mid-latitude site in the Himalayas.
Organic species were measured in solvent extracts of filter samples using gas chromatography–mass spectrometry (GCMS) and chemical derivatisation; this analysis was used to quantify molecular markers for primary aerosol sources – including motor vehicles, biomass burning and detritus – and SOA tracers.
Authentic standards of most SOA products were not commercially available at the time of this study, so surrogate standards were used for semiquantitation.
Using an empirical approach to uncertainty estimation based on homologous series of atmospherically relevant model compounds, analytical uncertainties ranged from 32 % for SOA tracers with structurally similar surrogates to more than 100 % for tracers with a poorly matched surrogate.
Biogenic SOA contributions to PM2.
5 organic carbon content in the 2005 monsoon and post-monsoon season ranged from 2–19 % for isoprene, 1–5 % for monoterpenes and 1–4 % for sesquiterpenes.
High concentrations of isoprene derivatives in aerosol, particularly in the late summer months, point to biogenic SOA as a significant source of organic carbon in the Himalayan region.
Related Results
Experimental studies on cloud condensation nuclei activation and cloud microphysical properties
Experimental studies on cloud condensation nuclei activation and cloud microphysical properties
Atmospheric aerosol particles have the ability to affect climate through cloud interactions and direct scattering and absorption of radiation. These aerosol particles can also affe...
Assessment of dynamic aerosol-radiation interaction in atmospheric models
Assessment of dynamic aerosol-radiation interaction in atmospheric models
In this thesis an assessment of the parameterization of the Aerosol-Radiation Interaction (ARI) in online integrated meteorology-chemistry models has been conducted. The model esti...
Decadal Characterization of Satellite-based Aerosol Types Over Arabian Peninsula: Comprehensive Insight and General Performance
Decadal Characterization of Satellite-based Aerosol Types Over Arabian Peninsula: Comprehensive Insight and General Performance
Retrieving aerosol characteristics such as particle size, shape, and absorption properties is a big challenge in satellite-based remote sensing, mainly for the single-viewing-angle...
Strong light scattering of highly oxygenated organic aerosols impacts significantly on visibility degradation
Strong light scattering of highly oxygenated organic aerosols impacts significantly on visibility degradation
Abstract. Secondary organic aerosols (SOAs) account for a large fraction of atmospheric
aerosol mass and play significant roles in visibility impairment by
scattering solar radiati...
Aerosol optical and radiative properties over Asia: Ground-based AERONET observations
Aerosol optical and radiative properties over Asia: Ground-based AERONET observations
Aerosols continue to contribute the largest uncertainty in quantifying Earth’s climate change. The uncertainty associated with aerosol radiative forcing is found to be hi...
Strong light scattering of highly oxygenated organic aerosols impacts significantly on visibility degradation
Strong light scattering of highly oxygenated organic aerosols impacts significantly on visibility degradation
Abstract. Secondary organic aerosols (SOA) account for a large fraction of atmospheric aerosol mass and play significant roles in visibility impairment by scattering solar radiatio...
A holistic aerosol model for Uranus and Neptune, including Dark Spots
A holistic aerosol model for Uranus and Neptune, including Dark Spots
<p>Previous studies of the reflectance spectra of Uranus and Neptune concentrated on individual, narrow wavelength regions, inferring solutions for the vertical struc...
The end of the anthropogenic aerosol era?
The end of the anthropogenic aerosol era?
<p>The Earth&#8217;s climate is rapidly changing. Over the past century, aerosols, via their ability to absorb or scatter solar radiation and alter clouds, pl...

