Articles | Volume 11, issue 4
https://doi.org/10.5194/esurf-11-547-2023
https://doi.org/10.5194/esurf-11-547-2023
Research article
 | 
06 Jul 2023
Research article |  | 06 Jul 2023

Synoptic-scale to mesoscale atmospheric circulation connects fluvial and coastal gravel conveyors and directional deposition of coastal landforms in the Dead Sea basin

Haggai Eyal, Moshe Armon, Yehouda Enzel, and Nadav G. Lensky

Viewed

Total article views: 1,604 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
1,132 385 87 1,604 144 70 75
  • HTML: 1,132
  • PDF: 385
  • XML: 87
  • Total: 1,604
  • Supplement: 144
  • BibTeX: 70
  • EndNote: 75
Views and downloads (calculated since 03 Nov 2022)
Cumulative views and downloads (calculated since 03 Nov 2022)

Viewed (geographical distribution)

Total article views: 1,604 (including HTML, PDF, and XML) Thereof 1,541 with geography defined and 63 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Latest update: 23 Nov 2024
Download
Short summary
Extracting paleoenvironmets from sedimentologic and geomorphic records is a main goal in Earth sciences. We study a chain of processes connecting causative Mediterranean cyclones, coeval floods, storm waves generated by mesoscale funneled wind, and coastal gravel transport. This causes northward dispersion of gravel along the modern Dead Sea coast, which has also persisted since the late Pleistocene, resulting in beach berms and fan deltas always being deposited north of channel mouths.