EGU21-12642, updated on 13 Jan 2023
https://doi.org/10.5194/egusphere-egu21-12642
EGU General Assembly 2021
© Author(s) 2023. This work is distributed under
the Creative Commons Attribution 4.0 License.

Understanding fluvial aggradation styles through physical modelling: Are we able to distinguish changes in water discharge and/or sediment supply (upstream drivers) from changes in base-level (downstream forcing) on river aggradation?  

Stephen E. Watkins1, Guy Simpson1, Laure Guerit2, Frédéric Arlaud1, Valentin Marguin1, Marine Prieur1, Nikhil Sharma1, Maxime Tremblin1, Luis Valero1, Abdallah S. Zaki1, and Sébastien Castelltort1
Stephen E. Watkins et al.
  • 1Department of Earth Sciences, University of Geneva, Geneva, Switzerland (stephen.watkins@unige.ch)
  • 2University of Rennes, CNRS, Géosciences Rennes, UMR 6118, France

How to cite: Watkins, S. E., Simpson, G., Guerit, L., Arlaud, F., Marguin, V., Prieur, M., Sharma, N., Tremblin, M., Valero, L., Zaki, A. S., and Castelltort, S.: Understanding fluvial aggradation styles through physical modelling: Are we able to distinguish changes in water discharge and/or sediment supply (upstream drivers) from changes in base-level (downstream forcing) on river aggradation?  , EGU General Assembly 2021, online, 19–30 Apr 2021, EGU21-12642, https://doi.org/10.5194/egusphere-egu21-12642, 2021.

This abstract has been withdrawn on 14 Apr 2021.