Articles | Volume 17, issue 7
https://doi.org/10.5194/acp-17-4627-2017
https://doi.org/10.5194/acp-17-4627-2017
Research article
 | 
07 Apr 2017
Research article |  | 07 Apr 2017

Annual variation in event-scale precipitation δ2H at Barrow, AK, reflects vapor source region

Annie L. Putman, Xiahong Feng, Leslie J. Sonder, and Eric S. Posmentier

Viewed

Total article views: 2,805 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
1,664 1,038 103 2,805 352 80 100
  • HTML: 1,664
  • PDF: 1,038
  • XML: 103
  • Total: 2,805
  • Supplement: 352
  • BibTeX: 80
  • EndNote: 100
Views and downloads (calculated since 11 Aug 2016)
Cumulative views and downloads (calculated since 11 Aug 2016)

Viewed (geographical distribution)

Total article views: 2,805 (including HTML, PDF, and XML) Thereof 2,801 with geography defined and 4 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Latest update: 17 Jul 2024
Download
Short summary
Water vapor source and transport are linked to the stable isotopes of precipitation of 70 storms at Barrow, AK, USA. Barrow's vapor came from the North Pacific in winter and the Arctic Ocean in summer. Half the isotopic variability was explained by the size of the temperature drop from the vapor source to Barrow, the evaporation conditions, and whether the vapor traveled over mountains. Because isotopes reflect the regional meteorology they may be early indicators of Arctic hydroclimatic change.
Altmetrics
Final-revised paper
Preprint