Temporal changes of inorganic ion deposition in the seasonal snow cover for the Austrian Alps (1983-2014)
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文摘

SO42−, NO3 and H+ in high alpine snow decrease over 30 years of observations.

Decrease in concentrations and depositions are lower than decrease in emissions.

Seasonal patterns show maximum concentrations during spring for NH4+, SO42− and H+.

Anthropogenic and crustal influence are the main sources for measured ions.

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