Sediment transport (dis)continuity across a beach–dune profile during an offshore wind event-Reference-Cited by-同舟云学术

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Sediment transport (dis)continuity across a beach–dune profile during an offshore wind event

Published:2015-09 Issue: Volume:245 Page:135-148
ISSN:0169-555X
Container-title:Geomorphology
language:en
Short-container-title:Geomorphology

Author:

Bauer Bernard O.^ORCID,Hesp Patrick A.,Walker Ian J.,Davidson-Arnott Robin G.D.

Funder

NSF

Publisher

Elsevier BV

Subject

Earth-Surface Processes

Reference65 articles.

1. Sediment supply from shoreface to dunes: linking sediment transport measurements and long term morphological evolution;Aagaard;Geomorphology,2004

2. The pattern of grainfall deposition in the lee of aeolian dunes;Anderson;Sedimentology,1988

3. Giant aeolian dune size determined by the average depth of the atmospheric boundary layer;Andreotti;Nature,2009

4. Numerical modelling of the wind flow over a transverse dune;Araújo;Sci. Rep.,2013

5. Patterns of sand transport on vegetated foredunes;Arens;Geomorphology,1996

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3. Skimming Flow and Sand Transport Within and Above Ammophila (Marram) Grass on a Foredune;Journal of Geophysical Research: Earth Surface;2023-06

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