The DOI matches its Crossref record.
Distribution of erosion across bedrock channels
Abstract
Lateral erosion in bedrock rivers is an important control on the shape of channel cross‐sections, and the coupling of channels and hillslopes. Recent observations link lateral erosion to the variability of flow. We propose two mechanisms to explain this. One is based on changing shear stress distributions within the channel with varying flood level, the other on the competition between cover and tool effects in fluvial bedrock erosion. We assess these processes for the Liwu River, Taiwan, and conclude that cover and tool effects dominate the partitioning of lateral and vertical erosion in this case. Copyright © 2007 John Wiley & Sons, Ltd.
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Cited by
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Hemingway, J. D., Hilton, R. G., Hovius, N., Eglinton, T. I., Haghipour, N., Wacker, L., Chen, M.-C., & Galy, V. V. (2018) · Science · doi:10.1126/science.aao6463 · Cited by 183
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Metadata
- Authors
- Turowski, J. M., Hovius, N., Meng‐Long, H., Lague, D., & Men‐Chiang, C.
- Venue
- Earth Surface Processes and Landforms
- Publisher
- Wiley
- Published
- 2007-07-18
- Volume
- 33
- Issue
- 3
- Pages
- 353-363
- ISSN
- 0197-9337 (ISSN-L)
- 1096-9837
- OpenAlex
- W2059531529
- Cited by
- 174
- References
- 0
- FWCI
- 7.39
- Type
- journal article
- Language
- en
- Open access
- closed
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- Turowski, J. M., Hovius, N., Meng‐Long, H., Lague, D., & Men‐Chiang, C. (2008). Distribution of erosion across bedrock channels. Earth Surface Processes and Landforms. https://doi.org/10.1002/esp.1559
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Contains information from the Semantic Scholar Academic Graph Datasets, made available under the ODC Attribution License (ODC-BY 1.0).
Semantic Scholar’s data is described in: Kinney, R., et al. (2023). The Semantic Scholar Open Data Platform. arXiv:2301.10140.
