Sinuosity evolution along an incising channel: New insights from the Jordan River response to the Dead Sea level fall

Author:

Dente Elad12ORCID,Lensky Nadav G.2ORCID,Morin Efrat1ORCID,Dunne Thomas3ORCID,Enzel Yehouda1ORCID

Affiliation:

1. The Fredy and Nadine Herrmann Institute of Earth Sciences; The Hebrew University of Jerusalem, Edmond J. Safra Campus; Givat Ram Jerusalem 91904 Israel

2. Geological Survey of Israel; 30 Malkhe Israel St. Jerusalem 95501 Israel

3. Bren School of Environmental Science and Management; University of California; Santa Barbara CA USA

Funder

Israel Science Foundation

Israeli Government

Publisher

Wiley

Subject

Earth and Planetary Sciences (miscellaneous),Earth-Surface Processes,Geography, Planning and Development

Reference66 articles.

1. Response of the Truckee River to lowering base level at Pyramid Lake, Nevada, based on historical air photos and LiDAR data;Adams;Geosphere,2012

2. Sink-to-source: influence of offshore dynamics on upstream processes;Abeyta;Basin Research,2018

3. Begin ZB Ehrlich A Nathan Y 1975 Lake Lisan, the Pleistocene precursor of the Dead Sea. Ministry of Commerce and Industry, Geological Survey of Israel

4. Development of longitudinal profiles of alluvial channels in response to base-level lowering;Begin;Earth Surface Processes and Landforms,1981

5. The morphotectonic structure of the lower Jordan Valley - an active segment of the Dead Sea Rift;Belitzky;Stephan Mueller Special Publication Series,2001

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