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Hygroscopic organic aerosols during BRAVO?
Douglas H Lowenthal1, Naresh Kumar, Jenny Hand
1Division of Atmospheric Sciences, Desert Research Institute, Reno, Nevada 89512, USA. dougl@dri.edu
Journal of the Air & Waste Management Association (1995)
|November 8, 2003
Summary
Organic aerosols
Area of Science:
- Atmospheric chemistry and physics
- Aerosol science
Background:
- The hygroscopic properties of organic aerosols, crucial for understanding their climate impact, remain poorly understood.
- Organic aerosols constitute a significant fraction (22% on average) of fine particulate matter (PM2.5).
Purpose of the Study:
- To investigate the water uptake of organic aerosols as a function of relative humidity (RH).
- To assess the contribution of organic aerosols to aerosol light scattering during the Big Bend Regional Aerosol and Visibility Observational Study (BRAVO).
Main Methods:
- Utilized data from the 1999 BRAVO field campaign.
- Estimated PM2.5 light scattering (Bsp) using aerosol chemical composition and dry particle size distributions at varying RH.
- Analyzed RH conditions, noting hourly RH exceeded 80% only 3.5% of the time, averaging 44%.
Main Results:
- Inorganic species' liquid water growth adequately explained measured PM2.5 light scattering (Bsp) at RH levels between 70% and 95%.
- The study focused on conditions where RH rarely exceeded 80%.
Conclusions:
- The contribution of organic aerosol hygroscopicity to light scattering may be less significant than previously assumed under the studied conditions.
- Further research is needed to fully elucidate the role of organic aerosols in atmospheric processes, particularly under high humidity conditions.