Event‐Scale Dynamics of a Parabolic Dune and Its Relevance for Mesoscale Evolution

Author:

Delgado‐Fernandez Irene1ORCID,Smyth Thomas A. G.23ORCID,Jackson Derek W. T.4ORCID,Smith Alexander B.5ORCID,Davidson‐Arnott Robin G. D.6ORCID

Affiliation:

1. Geography DepartmentEdge Hill University Ormskirk UK

2. Department of Geography and Environmental ScienceLiverpool Hope University Liverpool UK

3. Beach and Dune Systems Laboratory (BEADS), Faculty of Science and EngineeringFlinders University of South Australia Bedford Park South Australia Australia

4. Centre for Coastal and Marine Research, School of Environmental SciencesUniversity of Ulster Coleraine UK

5. Department of GeographyNational University of Ireland Galway Ireland

6. Department of GeographyUniversity of Guelph Guelph Ontario Canada

Funder

Natural Environment Research Council

Natural England

Publisher

American Geophysical Union (AGU)

Subject

Earth-Surface Processes,Geophysics

Reference64 articles.

1. American Meteorological Society(2018).Rain. Glossary of meteorology. Retrieved fromhttp://glossary.ametsoc.org/wiki/rain

2. Airflow and sand transport variations within a backshore–parabolic dune plain complex: NE Graham Island, British Columbia, Canada

3. Mobility of a remobilised parabolic dune in Kennemerland, The Netherlands

4. Ecogeomorphic state variables and phase‐space construction for quantifying the evolution of vegetated aeolian landscapes;Baas A. C. W.;Earth Surface Processes and Landforms,2010

5. From particle counts to flux: Wind tunnel testing and calibration of the ‘Wenglor’ aeolian sediment transport sensor

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