Gradual versus episodic lateral saltmarsh cliff erosion: Evidence from Terrestrial Laser Scans (TLS) and Surface Elevation Dynamics (SED) sensors-Reference-Cited by-同舟云学术

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Gradual versus episodic lateral saltmarsh cliff erosion: Evidence from Terrestrial Laser Scans (TLS) and Surface Elevation Dynamics (SED) sensors

Published:2023-04 Issue: Volume:426 Page:108590
ISSN:0169-555X
Container-title:Geomorphology
language:en
Short-container-title:Geomorphology

Author:

van der Wal Daphne^ORCID,van Dalen Jeroen,Willemsen Pim W.J.M.,Borsje Bas W.,Bouma Tjeerd J.

Publisher

Elsevier BV

Subject

Earth-Surface Processes

Reference82 articles.

1. Quantitative clay mineralogy as provenance indicator for recent muds in the southern North Sea;Adriaens;Mar. Geol.,2018

2. Evolution of salt-marsh cliffs in muddy and sandy systems: a qualitative comparison of British West-Coast estuaries;Allen;Earth Surf. Process. Landf.,1989

3. High spatio-temporal resolution measurements of cohesive sediment erosion;Beckers;Earth Surf. Process. Landf.,2020

4. On salt marshes retreat: experiments and modeling toppling failures induced by wind waves;Bendoni;J. Geophys. Res. Earth Surf.,2014

5. Insights into lateral marsh retreat mechanism through localized field measurements;Bendoni;Water Resour.Res.,2016

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