THE RATIO OF AEROSOL OPTICAL-ABSORPTION COEFFICIENTS TO SULFUR CONCENTRATIONS, AS AN INDICATOR OF SMOKE FROM FOREST-FIRES WHEN SAMPLING IN POLAR-REGIONS

Citation
Av. Polissar et al., THE RATIO OF AEROSOL OPTICAL-ABSORPTION COEFFICIENTS TO SULFUR CONCENTRATIONS, AS AN INDICATOR OF SMOKE FROM FOREST-FIRES WHEN SAMPLING IN POLAR-REGIONS, Atmospheric environment, 30(7), 1996, pp. 1147-1157
Citations number
18
Categorie Soggetti
Environmental Sciences","Metereology & Atmospheric Sciences
Journal title
ISSN journal
13522310
Volume
30
Issue
7
Year of publication
1996
Pages
1147 - 1157
Database
ISI
SICI code
1352-2310(1996)30:7<1147:TROAOC>2.0.ZU;2-8
Abstract
Analyses of aerosol composition data from seven National Park Service locations in Alaska were performed. All of the sampling sites in Alask a experience aerosol pollution from long distance and regional sources . One of the most important regional sources of particles in the area is wood smoke from forest fires. The Denali National Park aerosol data and the corresponding meteorological data made it possible to identif y samples of background (long-range-transported) aerosol, which are li kely to be without contamination from local and regional sources. Back ground values of optical absorption (BABS) and sulfur concentration fo r this site are well correlated and in ranges of 2 x 10(-7)-50 x 10(-7 ) m(-1) and 10-350 ng m(-3), respectively. Positive matrix factorizati on method was used for obtaining information about possible sources of aerosol in the remote locations. Seasonal variations with maxima duri ng the winter-spring season and minima in summer were observed for the sulfur concentration but not for BABS. Seasonal variations were alway s higher for the more northerly locations. The influence of emissions from regional sources on the BABS values was higher than for sulfur co ncentrations. The ratios of optical absorption coefficient to sulfur c oncentration were used to characterize the relative influence of regio nal pollution sources on the measured particle compositions.