Spatiotemporal model for the progression of transgressive dunes

Hezi Yizhaq*, Yosef Ashkenazy, Noam Levin, Haim Tsoar

*Corresponding author for this work

Research output: Contribution to journalArticlepeer-review

29 Scopus citations

Abstract

Transgressive dune fields, which are active sand areas surrounded by vegetation, exist on many coasts. In some regions like in Fraser Island in Australia, small dunes shrink while large ones grow, although both experience the same climatic conditions. We propose a general mathematical model for the spatiotemporal dynamics of vegetation cover on sand dunes and focus on the dynamics of transgressive dunes. Among other possibilities, the model predicts growth parallel to the wind with shrinkage perpendicular to the wind, where, depending on geometry and size, a transgressive dune can initially grow although eventually shrink. The larger is the initial area the slower its stabilization process. The model's predictions are supported by field observations from Fraser Island in Australia.

Original languageAmerican English
Pages (from-to)4502-4515
Number of pages14
JournalPhysica A: Statistical Mechanics and its Applications
Volume392
Issue number19
DOIs
StatePublished - 1 Oct 2013

Bibliographical note

Funding Information:
We thank the Israel Science Foundation for financial support.

Keywords

  • Climate change
  • Fraser
  • Island
  • Mathematical modeling
  • Transgressive dunes

Fingerprint

Dive into the research topics of 'Spatiotemporal model for the progression of transgressive dunes'. Together they form a unique fingerprint.

Cite this