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Miquel Mir-Gual, Guillem X. Pons, Irene Delgado-Fernández and Thomas A. G. Smyth
Blowouts are integral features of coastal dune fields. Their presence enhances both geomorphological and ecological diversity and enables the movement of sand by wind. Their role as a ?transport corridor? may be, however, considered negative from a coast...
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Zoran Kilibarda and Vesna Kilibarda
From 18 January 2013 (175.16 m a.s.l.) to 8 September 2020 (177.82 m a.s.l.), Lake Michigan experienced its fastest and highest rise (2.67 m) since 1860, when instrumental measurements began. Extensive foredunes developed since the last high lake levels ...
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Christiane Eichmanns and Holger Schüttrumpf
This study provides insights into dune toe growth around and between individual brushwood lines of sand trapping fences at the dune toe of coastal dunes using digital elevation models obtained from repeated unmanned aerial vehicle surveys. Prevailing bou...
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Jorn T. Tuijnman, Jasper J. A. Donker, Christian S. Schwarz and Gerben Ruessink
Wind-blown beach sand is the primary source for the volume growth of the most seaward dune, the foredune. Strong wind events can potentially dominate long-term aeolian supply but in reality do not contribute considerably because they often coincide with ...
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P. Soupy Dalyander, Rangley C. Mickey, Davina L. Passeri and Nathaniel G. Plant
Coastal zone managers require models that predict barrier island change on decadal time scales to estimate coastal vulnerability, and plan habitat restoration and coastal protection projects. To meet these needs, methods must be available for predicting ...
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Pam Hage, Gerben Ruessink, Zilla van Aartrijk and Jasper Donker
Transport of beach sand to the foredune by wind is essential for dunes to grow. The aeolian sand transport rate is related to wind velocity, but wind-based models often overpredict this transport for narrow beaches (<100 m). To better predict aeolian san...
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Christiane Eichmanns and Holger Schüttrumpf
For the restoration and maintenance of beach and dune systems along the coast, knowledge of aeolian sediment transport and its interaction with coastal protection measures is required. As a nature-based solution, sand trapping fences can be an integral p...
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Thomas B. Doyle, Andrew D. Short, Peter Ruggiero and Colin D. Woodroffe
Foredunes are important features within coastal landscapes, yet there are relatively few medium to long-term studies on how they evolve and change over time. This study of Australia?s New South Wales (NSW) foredunes has used 70 years of aerial photograph...
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Katherine Brodie, Ian Conery, Nicholas Cohn, Nicholas Spore and Margaret Palmsten
Coastal foredunes are topographically high features that can reduce vulnerability to storm-related flooding hazards. While the dominant aeolian, hydrodynamic, and ecological processes leading to dune growth and erosion are fairly well-understood, predict...
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Nicholas Cohn, Bas M. Hoonhout, Evan B. Goldstein, Sierd De Vries, Laura J. Moore, Orencio Durán Vinent and Peter Ruggiero
Coastal landscape change represents aggregated sediment transport gradients from spatially and temporally variable marine and aeolian forces. Numerous tools exist that independently simulate subaqueous and subaerial coastal profile change in response to ...
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