Aerosol chemical composition data for seven National Park Service loca
tions in Alaska for the period from 1986 to 1995 were analyzed. Data f
or elements, black carbon, and total mass were obtained for samples of
atmospheric particles less than 2.5 mu m in diameter. Assuming that a
ll elemental aerosol S was from SO4=, concentrations of excess (nonmar
ine) sulfate (XSO4=) were calculated by subtraction of the sea salt SO
4= mass fraction to Na and observed Na concentrations. Mass concentrat
ion of XSO4= ranged from 0.01 to 3.9 mu g m(-3), and mass concentratio
n of black carbon (BC) ranged from 0.01 to 5 mu g m(-3). Seasonal vari
ations with maxima during the winter/spring season and minima in the s
ummer for most of the sites in Alaska were observed for the XSO4= but
not for the BC and the fine mass concentration. The seasonal variation
s of XSO4= concentration were always higher in northwestern Alaska. BC
concentration in central Alaska peaked during the summertime because
of the high BC emission from forest fires. The Pb concentration in cen
tral Alaska shows a negative trend over the timescale of measurements.
It is concluded that all of the sites experience aerosol pollution fr
om long distance, regional, and local sources. Seasonal variations of
the XSO4= concentration are related to the seasonal variations in long
-range transport of midlatitudinal S emissions, to the varying rate of
photochemical SO4= fine aerosol production and to fine aerosol remova
l processes in the troposphere. The spatial distribution of XSO4= show
s a strong northwest to southeast negative gradient that can be associ
ated with the long-range transport of anthropogenic aerosol from pollu
tion sources located to the north or northwest of Alaska.