Vertical snow samples obtained from Murododaira (2450 m a. s. l.), Tateyama area of the Northern Alps, central Japan, were analyzed for ionic constituents to study chemical stratigraphy as archives of total deposition in winter to spring. Ionic constituents in the snow cover were divided into sea-salt (Na
+, Cl
-, Mg
2+), continental desert dust (KOSA) (Ca
2+, F
-, C
2O
42-, PO
43-), and anthropogenic pollution (NO
3-, SO
42-, NH
4+, nssK
+, Zn, H
+) components.
Several peaks in concentration profiles were significant in winter for sea-salt and in spring for KOSA components. Although pollution related species showed high concentrations in early winter and spring periods, their sporadic peaks were often correlated with KOSA components. Non sea-salt (nss) Ca
2+ concentration showed a good correlation with nssSr in the snow samples. According to comparison with Sr/Ca ratios in the literature, nssCa
2+ deposited on Murododaira in winter was considered to be originated from desert and loess areas in the east Asian continent. Average concentrations in spring snow cover from 1994 to 1999 showed large yearly variabilities (about twice) for sea-salt and KOSA components but were nearly constant for NO
3-, nssSO
42, NH
4+, and H
+.
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