Current address: R. Egozi, Division of Environmental, Water and Agricultural Engineering, Faculty of Civil and Environmental Engineering, Technion, Haifa 32000, Israel. Tel: +972-4-829-2625.
Defining and measuring braiding intensity
Article first published online: 24 APR 2008
Copyright © 2008 John Wiley & Sons, Ltd.
Earth Surface Processes and Landforms
Volume 33, Issue 14, pages 2121–2138, December 2008
How to Cite
Egozi, R. and Ashmore, P. (2008), Defining and measuring braiding intensity. Earth Surf. Process. Landforms, 33: 2121–2138. doi: 10.1002/esp.1658
- Issue published online: 26 NOV 2008
- Article first published online: 24 APR 2008
- Manuscript Accepted: 10 DEC 2007
- Manuscript Revised: 20 NOV 2007
- Manuscript Received: 19 JUN 2007
- Braiding index;
- gravel-bed river;
- channel pattern;
- physical model
Geomorphological studies of braided rivers still lack a consistent measurement of the complexity of the braided pattern. Several simple indices have been proposed and two (channel count and total sinuosity) are the most commonly applied. For none of these indices has there been an assessment of the sampling requirements and there has been no systematic study of the equivalence of the indices to each other and their sensitivity to river stage. Resolution of these issues is essential for progress in studies of braided morphology and dynamics at the scale of the channel network.
A series of experiments was run using small-scale physical models of braided rivers in a 3 m ∞ 20 m flume. Sampling criteria for braid indices and their comparability were assessed using constant-discharge experiments. Sample hydrographs were run to assess the effect of flow variability.
Reach lengths of at least 10 times the average wetted width are needed to measure braid indices with precision of the order of 20% of the mean. Inherent variability in channel pattern makes it difficult to achieve greater precision. Channel count indices need a minimum of 10 cross-sections spaced no further apart than the average wetted width of the river. Several of the braid indices, including total sinuosity, give very similar numerical values but they differ substantially from channel-count index values. Consequently, functional relationships between channel pattern and, for example, discharge, are sensitive to the choice of braid index. Braid indices are sensitive to river stage and the highest values typically occur below peak flows of a diurnal (melt-water) hydrograph in pro-glacial rivers. There is no general relationship with stage that would allow data from rivers at different relative stage to be compared. At present, channel count indices give the best combination of rapid measurement, precision, and range of sources from which measurements can be reliably made. They can also be related directly to bar theory for braided pattern development. Copyright © 2008 John Wiley & Sons, Ltd.