Embryo dune development on a large, actively accreting macrotidal beach: Calais, North Sea coast of France

Sediment budget data from an 18‐month topographic survey were analysed with data from brief experiments on wind parameters, beach moisture contents, bedforms and sand mobilization in order to monitor conditions and patterns of embryo dune development over a flat 150–1000 m wide accreting upper beach...

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Bibliographic Details
Published inEarth surface processes and landforms Vol. 32; no. 4; pp. 631 - 636
Main Authors Anthony, Edward J., Vanhée, Stéphane, Ruz, Marie-Hélène
Format Journal Article
LanguageEnglish
Published Chichester, UK John Wiley & Sons, Ltd 15.04.2007
Wiley
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Summary:Sediment budget data from an 18‐month topographic survey were analysed with data from brief experiments on wind parameters, beach moisture contents, bedforms and sand mobilization in order to monitor conditions and patterns of embryo dune development over a flat 150–1000 m wide accreting upper beach. The surface conditions over the upper beach locally affect aeolian transport, but net dune development over time depends on sustained strong winds and their orientation. Incoming marine sand supplied by storms and onshore winds is reorganized by the dominant offshore to longshore winds into elongated embryo dunes over this upper beach, imprinting a regional morphology of long‐term longshore dune ridge development. Copyright © 2006 John Wiley & Sons, Ltd.
Bibliography:ArticleID:ESP1442
istex:1057FAEA0509821BD5434F1C14D9A8B7208E0CEB
Nord-Pas-de-Calais Regional Council in Lille
ark:/67375/WNG-34GW6631-4
ObjectType-Article-1
SourceType-Scholarly Journals-1
ObjectType-Feature-2
content type line 23
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ISSN:0197-9337
1096-9837
DOI:10.1002/esp.1442