We present the evolution of multispectral optical properties through urban aerosols that have aged and interacted with biogenic emissions, resulting in stronger short wavelength absorption and the formation of moderately brown secondary organic aerosols. Ground-based aerosol measurements were made in June 2010 within the Sacramento urban area (site T0) and at a 40-km downwind location (site T1) in the forested Sierra Nevada foothills area. Data on black carbon (BC) and non-refractory aerosol mass and composition were collected at both sites. In addition, photoacoustic (PA) instruments with integrating nephelometers were used to measure spectral absorption and scattering coefficients for wavelengths ranging from 355 to 870 nm. The daytime ab...
In order to determine the wavelength dependence of fine (<1 micron) atmospheric aerosol absorptio...
Atmospheric black carbon (BC) and light absorbing organic aerosol (also referred as brown carbon, Br...
The aerosol spectral absorption efficiency (alpha(a) in m(2)/g) is measured over an extended wavelen...
We present the evolution of multispectral optical properties through urban aerosols that have aged a...
Ground-based aerosol measurements made in June 2010 within Sacramento urban area (site T0) and at a ...
Light-absorptivity of organic aerosol may play an important role in visibility and climate forcing, ...
Understanding the sources of light-absorbing organic (brown) carbon (BrC) and its interaction with b...
Knowledge gaps in the optical properties of carbonaceous aerosols account for a significant fraction...
The radiative impact of organic aerosols (OA) is a large source of uncertainty in estimating the glo...
The radiative impact of organic aerosols (OA) is a large source of uncertainty in estimating the glo...
Organic aerosols (OA) have long been thought to only scatter incoming solar radiation and have a coo...
Atmospheric black carbon (BC) and light-absorbing organic aerosol (also referred as brown carbon, Br...
In order to determine the wavelength dependence of fine (<1 micron) atmospheric aerosol absorptio...
Atmospheric black carbon (BC) and light absorbing organic aerosol (also referred as brown carbon, Br...
The aerosol spectral absorption efficiency (alpha(a) in m(2)/g) is measured over an extended wavelen...
We present the evolution of multispectral optical properties through urban aerosols that have aged a...
Ground-based aerosol measurements made in June 2010 within Sacramento urban area (site T0) and at a ...
Light-absorptivity of organic aerosol may play an important role in visibility and climate forcing, ...
Understanding the sources of light-absorbing organic (brown) carbon (BrC) and its interaction with b...
Knowledge gaps in the optical properties of carbonaceous aerosols account for a significant fraction...
The radiative impact of organic aerosols (OA) is a large source of uncertainty in estimating the glo...
The radiative impact of organic aerosols (OA) is a large source of uncertainty in estimating the glo...
Organic aerosols (OA) have long been thought to only scatter incoming solar radiation and have a coo...
Atmospheric black carbon (BC) and light-absorbing organic aerosol (also referred as brown carbon, Br...
In order to determine the wavelength dependence of fine (<1 micron) atmospheric aerosol absorptio...
Atmospheric black carbon (BC) and light absorbing organic aerosol (also referred as brown carbon, Br...
The aerosol spectral absorption efficiency (alpha(a) in m(2)/g) is measured over an extended wavelen...