The DOI matches its Crossref record.
Riparian vegetation as a primary control on channel characteristics in multi-thread rivers
Abstract
This chapter contains sections titled: Introduction Background and Methods Results Discussion ConclusionS
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Citations
Cited by
Pollen, N., & Simon, A. (2005) · Water Resources Research · doi:10.1029/2004wr003801 · Cited by 703
Parker, G., Wilcock, P. R., Paola, C., Dietrich, W. E., & Pitlick, J. (2007) · Journal of Geophysical Research: Earth Surface · doi:10.1029/2006jf000549 · Cited by 444
Self-citationEffects of vegetation on channel morphodynamics: results and insights from laboratory experiments
Tal, M., & Paola, C. (2010) · Earth Surface Processes and Landforms · doi:10.1002/esp.1908 · Cited by 396
Self-citationGravel-Bed Rivers VI: From Process Understanding to River Restoration
(2007) · Developments in Earth Surface Processes · doi:10.1016/s0928-2025(07)x1100-3 · Cited by 362
MODELING THE INTERACTIONS BETWEEN RIVER MORPHODYNAMICS AND RIPARIAN VEGETATION
Camporeale, C., Perucca, E., Ridolfi, L., & Gurnell, A. M. (2013) · Reviews of Geophysics · doi:10.1002/rog.20014 · Cited by 265
Metadata
- Authors
- Tal, M., Gran, K., Murray, A. B., Paola, C., & Hicks, D. M.
- Venue
- Water Science and Application
- Publisher
- American Geophysical Union
- Published
- 2004
- Pages
- 43-58
- ISSN
- 1526-758X (ISSN-L)
- OpenAlex
- W1547169465
- Cited by
- 187
- References
- 0
- FWCI
- 11.02
- Type
- book chapter
- Language
- en
- Open access
- closed
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- The paper
- Tal, M., Gran, K., Murray, A. B., Paola, C., & Hicks, D. M. (2004). Riparian vegetation as a primary control on channel characteristics in multi-thread rivers. Water Science and Application. https://doi.org/10.1029/008wsa04
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Bibliographic data: Semantic Scholar, OpenAlex, Crossref.
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.
