Articles | Volume 16, issue 11
https://doi.org/10.5194/acp-16-7435-2016
https://doi.org/10.5194/acp-16-7435-2016
Research article
 | 
15 Jun 2016
Research article |  | 15 Jun 2016

The role of dew as a night-time reservoir and morning source for atmospheric ammonia

Gregory R. Wentworth, Jennifer G. Murphy, Katherine B. Benedict, Evelyn J. Bangs, and Jeffrey L. Collett Jr.

Viewed

Total article views: 3,767 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
2,315 1,338 114 3,767 465 90 103
  • HTML: 2,315
  • PDF: 1,338
  • XML: 114
  • Total: 3,767
  • Supplement: 465
  • BibTeX: 90
  • EndNote: 103
Views and downloads (calculated since 07 Mar 2016)
Cumulative views and downloads (calculated since 07 Mar 2016)

Cited

Saved (preprint)

Discussed (final revised paper)

Latest update: 14 Dec 2024
Download
Short summary
The influence of dew on atmospheric composition is poorly understood. Results from this work show that dew can uptake a significant fraction (roughly two-thirds) of boundary layer gas-phase ammonia. Furthermore, an average of 95 % of the ammonia sequestered in dew is released back to the atmosphere the following morning during dew evaporation. Dew has the ability to affect air quality and N-deposition and should be considered when modelling ammonia concentrations, as well as other soluble gases.
Altmetrics
Final-revised paper
Preprint