Articles | Volume 4, issue 3
https://doi.org/10.5194/wcd-4-725-2023
https://doi.org/10.5194/wcd-4-725-2023
Research article
 | 
31 Aug 2023
Research article |  | 31 Aug 2023

Adverse impact of terrain steepness on thermally driven initiation of orographic convection

Matthias Göbel, Stefano Serafin, and Mathias W. Rotach

Viewed

Total article views: 3,858 (including HTML, PDF, and XML)
HTML PDF XML Total BibTeX EndNote
2,784 961 113 3,858 168 292
  • HTML: 2,784
  • PDF: 961
  • XML: 113
  • Total: 3,858
  • BibTeX: 168
  • EndNote: 292
Views and downloads (calculated since 06 Apr 2023)
Cumulative views and downloads (calculated since 06 Apr 2023)

Viewed (geographical distribution)

Total article views: 3,858 (including HTML, PDF, and XML) Thereof 3,783 with geography defined and 75 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Saved (final revised paper)

Latest update: 05 Jun 2026
Download
Short summary
On summer days over mountains, upslope winds transport moist air towards mountain tops and beyond, making local rain showers more likely. We use idealized simulations to investigate how mountain steepness affects this mechanism. We find that steeper mountains lead to a delayed onset and lower intensity of the storms, because less moisture accumulates over the ridges and the thermal updraft zone at the top is narrower and thus more prone to the intrusion of dry air from the environment.
Share