Articles | Volume 2, issue 1
https://doi.org/10.5194/wcd-2-37-2021
https://doi.org/10.5194/wcd-2-37-2021
Research article
 | 
18 Jan 2021
Research article |  | 18 Jan 2021

Mid-level convection in a warm conveyor belt accelerates the jet stream

Nicolas Blanchard, Florian Pantillon, Jean-Pierre Chaboureau, and Julien Delanoë

Viewed

Total article views: 1,714 (including HTML, PDF, and XML)
HTML PDF XML Total BibTeX EndNote
1,169 494 51 1,714 47 32
  • HTML: 1,169
  • PDF: 494
  • XML: 51
  • Total: 1,714
  • BibTeX: 47
  • EndNote: 32
Views and downloads (calculated since 16 Oct 2020)
Cumulative views and downloads (calculated since 16 Oct 2020)

Viewed (geographical distribution)

Total article views: 1,714 (including HTML, PDF, and XML) Thereof 1,630 with geography defined and 84 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Latest update: 30 Oct 2024
Download
Short summary
Rare aircraft observations in the warm conveyor belt outflow associated with an extratropical cyclone are complemented with convection-permitting simulations. They reveal a complex tropopause structure with two jet stream cores, from which one is reinforced by bands of negative potential vorticity. They show that negative potential vorticity takes its origin in mid-level convection, which indirectly accelerates the jet stream and, thus, may influence the downstream large-scale circulation.