Articles | Volume 14, issue 23
https://doi.org/10.5194/acp-14-12763-2014
https://doi.org/10.5194/acp-14-12763-2014
Research article
 | 
05 Dec 2014
Research article |  | 05 Dec 2014

Surface-to-mountaintop transport characterised by radon observations at the Jungfraujoch

A. D. Griffiths, F. Conen, E. Weingartner, L. Zimmermann, S. D. Chambers, A. G. Williams, and M. Steinbacher

Viewed

Total article views: 3,492 (including HTML, PDF, and XML)
HTML PDF XML Total BibTeX EndNote
2,297 1,093 102 3,492 101 95
  • HTML: 2,297
  • PDF: 1,093
  • XML: 102
  • Total: 3,492
  • BibTeX: 101
  • EndNote: 95
Views and downloads (calculated since 04 Jul 2014)
Cumulative views and downloads (calculated since 04 Jul 2014)

Cited

Saved (final revised paper)

Saved (preprint)

Latest update: 24 Apr 2024
Download
Short summary
Radon detectors at Bern and Jungfraujoch were used to monitor the transport of radon-rich boundary layer air from the Swiss Plateau to the Alpine ridge. Radon was successfully used to discriminate between different types of vertical transport, using the shape of the diurnal cycle to identify days with upslope mountain winds. For many air-mass properties, however, the total land-surface influence (indicated by the radon concentration) was more decisive than the type of vertical transport.
Altmetrics
Final-revised paper
Preprint