A reduced-complexity shoreline change model combining longshore and cross-shore processes: The LX-Shore model. Robinet, A., Idier, D., Castelle, B., & Marieu, V. 109:1–16. ![A reduced-complexity shoreline change model combining longshore and cross-shore processes: The LX-Shore model [link]](https://bibbase.org/img/filetypes/link.svg "link")
Paper doi abstract bibtex A reduced-complexity numerical model, LX-Shore, is developed to simulate shoreline evolution along wave-dominated sandy coasts. The model can handle any sandy shoreline geometries (e.g. sand spits, islands), including non-erodible areas such as coastal defenses and headlands, and is coupled with a spectral wave model to cope with complex nearshore wave fields. Shoreline change is primarily driven by the gradients in total longshore sediment transport and by the cross-shore transport owing to variability in incident wave energy. Application to academic cases and a real coast highlights the potential of LX-Shore to simulate shoreline change on timescales from hours (storm) to decades with low computational cost. LX-Shore opens new perspectives in terms of knowledge on the primary mechanisms locally driving shoreline change and for ensemble-based simulations of future shoreline evolution.
@article{robinet_reduced-complexity_2018,
title = {A reduced-complexity shoreline change model combining longshore and cross-shore processes: The {LX}-Shore model},
volume = {109},
issn = {1364-8152},
url = {http://www.sciencedirect.com/science/article/pii/S136481521731085X},
doi = {10.1016/j.envsoft.2018.08.010},
shorttitle = {A reduced-complexity shoreline change model combining longshore and cross-shore processes},
abstract = {A reduced-complexity numerical model, {LX}-Shore, is developed to simulate shoreline evolution along wave-dominated sandy coasts. The model can handle any sandy shoreline geometries (e.g. sand spits, islands), including non-erodible areas such as coastal defenses and headlands, and is coupled with a spectral wave model to cope with complex nearshore wave fields. Shoreline change is primarily driven by the gradients in total longshore sediment transport and by the cross-shore transport owing to variability in incident wave energy. Application to academic cases and a real coast highlights the potential of {LX}-Shore to simulate shoreline change on timescales from hours (storm) to decades with low computational cost. {LX}-Shore opens new perspectives in terms of knowledge on the primary mechanisms locally driving shoreline change and for ensemble-based simulations of future shoreline evolution.},
pages = {1--16},
journaltitle = {Environmental Modelling \& Software},
shortjournal = {Environmental Modelling \& Software},
author = {Robinet, Arthur and Idier, Déborah and Castelle, Bruno and Marieu, Vincent},
urldate = {2019-11-26},
date = {2018-11-01},
langid = {english},
keywords = {Shoreline change, Numerical model, Cross-shore transport, Longshore transport, Sandy coasts}
}
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