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Estimating reach-averaged discharge for the River Severn from measurements of river water surface elevation and slope
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“The scaling coefficient a and the hydraulic exponent b encapsulate the combined effects of channel geometry and roughness: b reflects the shape of the cross-section (e.g., b = 5/3 for a wide rectangular channel under Manning’s equation54), while a integrates the effects of channel roughness, bed slope, and geometry.”
From Global scale river discharge and mean depth from radar altimetry and model (2026) · cites this paper as [54]
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Cited by
The SWOT Mission and Its Capabilities for Land Hydrology
Biancamaria, S., Lettenmaier, D. P., & Pavelsky, T. M. (2016) · Surveys in Geophysics · doi:10.1007/s10712-015-9346-y · Cited by 458
Global scale river discharge and mean depth from radar altimetry and model
Paris, A., Garambois, P.-A., Gal, L., Cerbelaud, A., Larnier, K., David, C. H., Jucá Oliveira, R. A., Correa, S. W., Tourian, M. J., & Calmant, S. (2026) · Nature Communications · doi:10.1038/s41467-026-78275-5
Metadata
- Authors
- Durand, M., Neal, J., Rodríguez, E., Andreadis, K. M., Smith, L. C., & Yoon, Y.
- Venue
- Journal of Hydrology
- Publisher
- Elsevier BV
- Published
- 2014-04
- Volume
- 511
- Pages
- 92-104
- ISSN
- 0022-1694
- Cited by
- 155
- References
- 1
- Language
- en
- Licence
- www.elsevier.com/tdm/userlicense/1.0/ (tdm)
- www.elsevier.com/legal/tdmrep-license (tdm)
- www.elsevier.com/open-access/userlicense/1.0/ (am, 295 d)
- doi.org/10.15223/policy-017 (stm-asf)
- doi.org/10.15223/policy-037 (stm-asf)
- doi.org/10.15223/policy-012 (stm-asf)
- doi.org/10.15223/policy-029 (stm-asf)
- doi.org/10.15223/policy-004 (stm-asf)
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- The paper
- Durand, M., Neal, J., Rodríguez, E., Andreadis, K. M., Smith, L. C., & Yoon, Y. (2014). Estimating reach-averaged discharge for the River Severn from measurements of river water surface elevation and slope. Journal of Hydrology. https://doi.org/10.1016/j.jhydrol.2013.12.050
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