The rain and snow samples were collected at the summit (3776m) and Tarobo (1300m) of Mt. Fuji from Aug., 1990 to July, 1992 in order to evaluate the ion concentrations of chemical species in precipitation. Generally, the concentrations of all the chemical species were lower at the summit than at Tarobo. The following relations were found between the ion concentrations and the pressure patterns. At the summit, the concentrations of nssSO
42- and NO
4- were very low for the precipitations caused from low passings along coast of Japan and Typhoons when air mass above the Pacific Oecean would be brought to Mt. Fuji. At Tarobeo, however, the ion concentrations were above 6 μeq 1
-1 for nssSO
32- and above 5 μeq1
-1 for NONO
3- in most cases of these pressure patterns. This result indicates that precipitation collected at the elevaiton of 1300m would be affected by short-distance transport from urban regions. The ion concentration of NO
3- was high at Tarobo in the case of northeasterly type of pressure pattern, suggesting advection of pollutants originated from the metropolitan area. Precipitations at Baiu showed markedly high values of nssSO
42- and NO
3- concentra tions at both elevations.
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