Progress toward clean cloud water at Whiteface Mountain New York

Fossil fuel combustion is the primary source of anthropogenic acidity in cloud water. Since 1994 there is a measurable decrease in hydrogen, sulfate, and nitrate ion concentrations in cloud water collected at Whiteface Mountain. In this paper we assess these changes from the point of view of progress toward clean air conditions. eanest clouds crossing Whiteface Mountain, those with the lowest total ion concentrations, are found to have pH values in the range 5.0–5.25. Furthermore, there is a linear relationship between pH, sulfate and nitrate ion concentrations in cloud water. With this in mind, we define clean cloud water values of sulfate, nitrate and hydrogen as mean concentrations observed in cloud water samples with pH in the range 5.0–5.25. n compare mean annual values to clean air values to determine annual ratios. In 1994, ratios for SO 4 2 − , NO 3 − and H+ were respectively 26.9, 13.1 and 29.9 times above the clean air value. In 2009, the SO 4 2 − , NO 3 − and H+ corresponding ratios were 4.2, 2.7, and 4.8 times above the clean air value. In other words, comparison of the 1994 and 2009 results suggest reductions in anthropogenic concentrations of SO 4 2 − , NO 3 − and H+, by 84%, 79% and 84% respectively. ify our approach, we have calculated corresponding changes in the aerosol SO 4 2 − ratio, with clean air concentrations equal to the natural background aerosol SO 4 2 − value used for the Regional Haze Rule. These results compared favorably to our cloud water SO 4 2 − ratio.