Observation of the whole process of interaction between barchans by flume experiments
- 22 June 2004
- journal article
- Published by American Geophysical Union (AGU) in Geophysical Research Letters
- Vol. 31 (12)
- https://doi.org/10.1029/2004gl020168
Abstract
Through laboratory experiments generating unidirectional water flows, we examine the process of interaction between two moving barchans (sandy bed configurations in a crescentic plan‐shape), which may take dozens of years for barchan dunes in the nature. Three types of the interaction were observed. The first type was absorption of two barchans into one. The second was that the upstream fast barchan rode on the downstream slow barchan and simultaneously a newly born barchan was ejected from the lee side of the slow barchan. The third was that the downstream slow barchan was split into two before the upstream fast barchan touched the downstream. The type of the interaction was determined by both relative and absolute size of two barchans.This publication has 11 references indexed in Scilit:
- Corridors of barchan dunes: Stability and size selectionPhysical Review E, 2004
- Barchan‐shaped ripple marks in a wave flumeEarth Surface Processes and Landforms, 2004
- Solitary wave behaviour of sand dunesNature, 2003
- Relevant Length Scale of Barchan DunesPhysical Review Letters, 2002
- Modelling a dune fieldPhysica A: Statistical Mechanics and its Applications, 2002
- Simulation of the effect of wind speedup in the formation of transverse dune fieldsEarth Surface Processes and Landforms, 2000
- Width, height and slope relationships and aerodynamic maintenance of barchansGeomorphology, 1998
- A Simple Model for the Various Pattern Dynamics of DunesInternational Journal of Modern Physics B, 1998
- Morphology and distribution of common ‘sand’ dunes on Mars: Comparison with the EarthJournal of Geophysical Research, 1979
- GEOLOGICAL STUDIES ON THE GREAT BAHAMA BANKPublished by Society for Sedimentary Geology ,1957