Articles | Volume 19, issue 24
https://doi.org/10.5194/acp-19-15199-2019
https://doi.org/10.5194/acp-19-15199-2019
Research article
 | 
16 Dec 2019
Research article |  | 16 Dec 2019

The role of spring dry zonal advection in summer drought onset over the US Great Plains

Amir Erfanian and Rong Fu

Viewed

Total article views: 2,005 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
1,325 626 54 2,005 254 58 49
  • HTML: 1,325
  • PDF: 626
  • XML: 54
  • Total: 2,005
  • Supplement: 254
  • BibTeX: 58
  • EndNote: 49
Views and downloads (calculated since 08 Apr 2019)
Cumulative views and downloads (calculated since 08 Apr 2019)

Viewed (geographical distribution)

Total article views: 2,005 (including HTML, PDF, and XML) Thereof 1,782 with geography defined and 223 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Latest update: 20 Nov 2024
Download
Short summary
An eastward advection of dry and warm air in spring was identified as a major drought onset mechanism over the US Great Plains (GP). Further breakdown of the zonal advection into the dynamic versus thermodynamic contributions revealed dominance of the latter in the tropospheric drying observed during the onset of GP 2011 and 2012 droughts. The dependence of thermodynamic advection on moisture gradient links the spring precipitation in the Rockies and US southwest to the GP summer precipitation.
Altmetrics
Final-revised paper
Preprint