Chemistry of Rainwater and Cloud Water at Remote Sites in Alaska and Oregon
- 1 April 1989
- journal article
- research article
- Published by Wiley in Journal of Environmental Quality
- Vol. 18 (2) , 149-152
- https://doi.org/10.2134/jeq1989.00472425001800020003x
Abstract
Cloud water and rainwater were examined at remote sites in southeastern Alaska and coastal Oregon using standardized collection and analytical techniques. Cloud water and rainwater were characterized by extremely low concentrations of most ions except SO2−4, Na+, and Cl−. Acidity was greater than expected because of organic acids from unknown sources. Concentrations of NO−3 and NH+4 were extremely low, especially compared to samples collected similarly in the eastern USA. Rainwater did not differ between Alaska and Oregon except in concentrations of Ca2+, Mg2+, K+, Na+, and Cl−. Cloud water generally had higher concentrations of ions than rainwater, especially in NO−3, NH+4, and SO2−4. Ion concentrations were highly variable and non‐normally distributed. Sample sizes in future studies should be large (>40). Cloud water deposition may be very important in terms of potential pollution effects and nutrient cycling in ecosystems with frequent cloud cover.This publication has 3 references indexed in Scilit:
- Cloudwater chemistry from ten sites in North AmericaEnvironmental Science & Technology, 1988
- Cloud Droplet Deposition in Subalpine Balsam Fir Forests: Hydrological and Chemical InputsScience, 1982
- The Calcium, Magnesium, Potassium, and Sodium Budgets for a Small Forested EcosystemEcology, 1967