Carbonaceous aerosols affect air quality and climate, but measurements of black (BC) and organic (OC) carbon concentrations are very uncertain. Many variants of the thermal-optical analysis (TOA) method exist, and more than a decade of research has not resolved the differences in their estimates of OC and BC (i.e., the OC/BC split). This is largely due to the lack of a BC standard. Without a BC standard, the accuracy of TOA measurements of OC and BC cannot be determined. The research goal is to develop a method of producing BC standards that can be used to determine the accuracy in TOA measurements of OC and BC. The uncertainty in TOA measurements is due to the presence of both OC and BC in particulate matter. Whereas measuring total carbon...
The replacement of the Desert Research Institute (DRI) model 2001 with model 2015 thermal/optical an...
We report on an inter-comparison of black-carbon- and aerosol-absorption-measuring instruments with ...
Aerosol direct radiative forcing on climate is significant but highly uncertain. Carbonaceous aeroso...
Black carbon (BC), a main component of combustion-generated soot, is a strong absorber of sunlight a...
Elemental Carbon (EC), also called Black Carbon (BC) when it is measured by optical techniques, is t...
Measurements of carbonaceous aerosols are of vital importance for local, regional and global air qua...
Carbonaceous aerosols play an important role in the atmosphere as they are responsible for visibilit...
The climatic impacts of black carbon (BC) aerosol, an important absorber of solar radiation in the a...
Comparison of black carbon (BC) measurements obtained by two methods was performed for aerosols samp...
Carbonaceous fraction of atmospheric particulate matter (PM), generally ranging between 20% and 50% ...
Soot particles, consisting of black carbon (BC), organic carbon (OC), inorganic salts, and trace ele...
Thermal-optical analysis is a conventional method for determining the carbonaceous aerosol fraction ...
Thermal/optical methods are widely used in the determination of aerosol organic carbon (OC) and elem...
Carbonaceous aerosol (CA) plays an important role in environmental issues like air quality, human he...
The replacement of the Desert Research Institute (DRI) model 2001 with model 2015 thermal/optical an...
The replacement of the Desert Research Institute (DRI) model 2001 with model 2015 thermal/optical an...
We report on an inter-comparison of black-carbon- and aerosol-absorption-measuring instruments with ...
Aerosol direct radiative forcing on climate is significant but highly uncertain. Carbonaceous aeroso...
Black carbon (BC), a main component of combustion-generated soot, is a strong absorber of sunlight a...
Elemental Carbon (EC), also called Black Carbon (BC) when it is measured by optical techniques, is t...
Measurements of carbonaceous aerosols are of vital importance for local, regional and global air qua...
Carbonaceous aerosols play an important role in the atmosphere as they are responsible for visibilit...
The climatic impacts of black carbon (BC) aerosol, an important absorber of solar radiation in the a...
Comparison of black carbon (BC) measurements obtained by two methods was performed for aerosols samp...
Carbonaceous fraction of atmospheric particulate matter (PM), generally ranging between 20% and 50% ...
Soot particles, consisting of black carbon (BC), organic carbon (OC), inorganic salts, and trace ele...
Thermal-optical analysis is a conventional method for determining the carbonaceous aerosol fraction ...
Thermal/optical methods are widely used in the determination of aerosol organic carbon (OC) and elem...
Carbonaceous aerosol (CA) plays an important role in environmental issues like air quality, human he...
The replacement of the Desert Research Institute (DRI) model 2001 with model 2015 thermal/optical an...
The replacement of the Desert Research Institute (DRI) model 2001 with model 2015 thermal/optical an...
We report on an inter-comparison of black-carbon- and aerosol-absorption-measuring instruments with ...
Aerosol direct radiative forcing on climate is significant but highly uncertain. Carbonaceous aeroso...