Long-term changes (1990–2015) in the atmospheric deposition and runoff water chemistry of sulphate, inorganic nitrogen and acidity for forested catchments in Europe in relation to changes in emissions and hydrometeorological conditions

Long-term changes (1990–2015) in the atmospheric deposition and runoff water chemistry of... •Trends in runoff fluxes of SO4 have increasingly responded to the decrease in S emissions.•Trends in NO3 concentrations in deposition and runoff are predominantly decreasing.•Trends in inorganic N output fluxes are still highly variable.•Variation of SO4 in runoff was most powerfully explained by deposition pattern.•No clear signs of a consistent climate-driven increase in inorganic N loss in forest catchments http://www.deepdyve.com/assets/images/DeepDyve-Logo-lg.png Science of the Total Environment Elsevier

Long-term changes (1990–2015) in the atmospheric deposition and runoff water chemistry of sulphate, inorganic nitrogen and acidity for forested catchments in Europe in relation to changes in emissions and hydrometeorological conditions

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Publisher
Elsevier
Copyright
Copyright © 2017 Elsevier B.V.
ISSN
0048-9697
eISSN
1879-1026
D.O.I.
10.1016/j.scitotenv.2017.12.245
Publisher site
See Article on Publisher Site

Abstract

•Trends in runoff fluxes of SO4 have increasingly responded to the decrease in S emissions.•Trends in NO3 concentrations in deposition and runoff are predominantly decreasing.•Trends in inorganic N output fluxes are still highly variable.•Variation of SO4 in runoff was most powerfully explained by deposition pattern.•No clear signs of a consistent climate-driven increase in inorganic N loss in forest catchments

Journal

Science of the Total EnvironmentElsevier

Published: Jun 1, 2018

References

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