@article {Dente2018,
	title = {Sinuosity evolution along an incising channel: New insights from the Jordan River response to the Dead Sea level fall},
	journal = {Earth Surface Processes and Landforms},
	year = {2018},
	abstract = {channel, increasing sinuosity. Upstream, near the migrating knickzone channel gradients also increase, incision is more moderate and floods continue to overtop the banks, favoring meander chute cutoffs. The resulting channel has a downstream well-confined meandering segment and an upstream low-sinuosity segment. These new insights regarding spatial differences along an incising channel can improve interpretations of the evolution of ancient planforms and floodplains that responded to base-level decline.},
	issn = {01979337},
	doi = {10.1002/esp.4530},
	url = {http://doi.wiley.com/10.1002/esp.4530},
	author = {Dente, Elad and Lensky, Nadav G. and Morin, Efrat and Dunne, Thomas and Enzel, Yehouda}
}
