Articles | Volume 17, issue 9
https://doi.org/10.5194/acp-17-6113-2017
https://doi.org/10.5194/acp-17-6113-2017
Research article
 | 
17 May 2017
Research article |  | 17 May 2017

Enhanced stratospheric water vapor over the summertime continental United States and the role of overshooting convection

Robert L. Herman, Eric A. Ray, Karen H. Rosenlof, Kristopher M. Bedka, Michael J. Schwartz, William G. Read, Robert F. Troy, Keith Chin, Lance E. Christensen, Dejian Fu, Robert A. Stachnik, T. Paul Bui, and Jonathan M. Dean-Day

Viewed

Total article views: 2,919 (including HTML, PDF, and XML)
HTML PDF XML Total BibTeX EndNote
1,822 1,017 80 2,919 76 80
  • HTML: 1,822
  • PDF: 1,017
  • XML: 80
  • Total: 2,919
  • BibTeX: 76
  • EndNote: 80
Views and downloads (calculated since 19 Dec 2016)
Cumulative views and downloads (calculated since 19 Dec 2016)

Viewed (geographical distribution)

Total article views: 2,919 (including HTML, PDF, and XML) Thereof 2,947 with geography defined and -28 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Latest update: 17 Apr 2024
Download
Short summary
This study reports new aircraft field observations of elevated water vapor greater than 10 ppmv in the overworld stratosphere over the summertime continental US. Back trajectories from the flight track intersect overshooting convective tops within the previous 1 to 7 days, suggesting that ice is convectively and irreversibly transported to the stratosphere in the most energetic overshooting convective events. Satellite measurements (Aura MLS) indicate that such events are uncommon (< 1 %).
Altmetrics
Final-revised paper
Preprint