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Hydrol. Earth Syst. Sci., 6, 773-781, 2002
www.hydrol-earth-syst-sci.net/6/773/2002/
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Long-term response in episodic acidification to declining SO42– deposition in two streams in Nova Scotia

H. Laudon1,2, T. A. Clair3, and H. F. Hemond1
1Ralph M. Parsons Laboratory, Department of Civil and Environmental Engineering, MIT, Cambridge, MA, 02139, USA
2Present address: Department of Forest Ecology, Swedish University of Agricultural Sciences, 901 83 Umeå, Sweden
3Environment Canada, Atlantic Region, PO Box 6227, Sackville, N. B. E4L 1G6, Canada
E-mail for corresponding author: Hjalmar.Laudon@sek.slu.se

Abstract. Trends in anthropogenically driven episodic acidification associated with extended winter snow melt/rain episodes between 1983 and 1998 were investigated for two streams in Nova Scotia, Canada. The anthropogenic contribution to Acid Neutralization Capacity (ANC) was analysed using the Boreal Dilution Model (Bishop et al., 2000) modified by applying a sea-salt correction to all input hydrochemistry. The anthropogenic contribution to episodic ANC decline was statistically significant and strongly correlated with the decline in acid deposition, which decreased by approximately 50% during the period of record. Sensitivity analysis demonstrated that the BDM can be applied to surface waters with sea-salt contributions although the correction increases model uncertainty. Results of this study demonstrate the effectiveness of reduced emissions in North America in the last decades in decreasing the severity of episodic acidification in the Atlantic region of Canada.

Keywords: episodic acidification, acidification recovery, Nova Scotia, snowmelt, winter



Final Revised Paper (PDF, 661 KB)

Citation: Laudon, H., Clair, T. A., and Hemond, H. F.: Long-term response in episodic acidification to declining SO42– deposition in two streams in Nova Scotia, Hydrol. Earth Syst. Sci., 6, 773-781, 2002.   Bibtex   EndNote   Reference Manager