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Eolian dunes: Computer simulations and attractor interpretation
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1995
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GeophysicsAttractor InterpretationAeolian ProcessEngineeringMorphodynamicsGeomorphologyDepositional ProcessGeographyBeach DynamicEolian DunesGeologyComplex SystemsEarth SciencesGeological ModelingSedimentologyEarth SciencePlanetary GeomorphologyGeodesy
Research Article| December 01, 1995 Eolian dunes: Computer simulations and attractor interpretation B. T. Werner B. T. Werner 1Institute of Geophysics and Planetary Physics, University of California, San Diego, La Jolla, California 92093-0225 Search for other works by this author on: GSW Google Scholar Author and Article Information B. T. Werner 1Institute of Geophysics and Planetary Physics, University of California, San Diego, La Jolla, California 92093-0225 Publisher: Geological Society of America First Online: 02 Jun 2017 Online ISSN: 1943-2682 Print ISSN: 0091-7613 Geological Society of America Geology (1995) 23 (12): 1107–1110. https://doi.org/10.1130/0091-7613(1995)023<1107:EDCSAA>2.3.CO;2 Article history First Online: 02 Jun 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn MailTo Tools Icon Tools Get Permissions Search Site Citation B. T. Werner; Eolian dunes: Computer simulations and attractor interpretation. Geology 1995;; 23 (12): 1107–1110. doi: https://doi.org/10.1130/0091-7613(1995)023<1107:EDCSAA>2.3.CO;2 Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Search Dropdown Menu toolbar search search input Search input auto suggest filter your search All ContentBy SocietyGeology Search Advanced Search Abstract A simple computer-simulation algorithm for the transport of sand by wind produces forms resembling barchan, crescentic ridge, linear, and star natural dune classes. Sand is moved as slabs composed of many grains that are picked up at random, transported in a specified direction, and deposited (1) with a probability that depends on the local presence or absence of sand or (2) in shadow zones in the lee of dunes. The simulated dune fields are interpreted as complex systems, with sand-dune classes being dynamical attractors of these systems. The evolution of dunes once formed becomes decoupled from the details of eolian sand transport. This content is PDF only. Please click on the PDF icon to access. First Page Preview Close Modal You do not have access to this content, please speak to your institutional administrator if you feel you should have access.