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

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Cited articles

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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.
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