Snowcover surveys were carried out in Hokkaido, northern Japan. Snowpack sa
mples were collected using a steel pipe at 80 sites in 1988, 69 sites in 19
92, and 66 sites in 1996 and 2000 during the time when the water equivalent
s of the snowcover are the greatest Spatial distribution maps of water equi
valents and of the concentrations arid the accumulated amounts of hydrogen,
non-sea-salt sulfate and non-sea-salt calcium ion of the snowcover drawn b
y Kriging method are discussed.
The distribution maps show that water equivalents and the accumulated amoun
ts of hydrogen and non-sea-salt sulfate in all the sample years were larges
t in the Japan Sea region, as were the ion concentrations of hydrogen and n
on-sea-salt sulfate. It was estimated this was caused by air pollutants tra
nsported from a great distance. The ratio of areas below pH 5.0 increased t
emporally from 1988 (20%) to 1992, 1996 and 2000 (66-80%). This trend was e
stimated to be affected by a decline of non-sea-salt calcium concentrations
derived from alkaline road dust. In addition, the effect of snowcover comp
onents was assessed by comparison between the acid loads of the snowcover a
nd the acid neutralizing capacity of lake water. We found that lakes in the
middle of the Japan Sea coast have the potential to be acidified by snowme
lt.