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Hydraulics of floods upstream of horseshoe canyons and waterfalls

Lapotre, Mathieu G. A. and Lamb, Michael P. (2015) Hydraulics of floods upstream of horseshoe canyons and waterfalls. Journal of Geophysical Research. Earth Surface, 120 (7). pp. 1227-1250. ISSN 2169-9003. http://resolver.caltech.edu/CaltechAUTHORS:20150910-135122139

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Abstract

Horseshoe waterfalls are ubiquitous in natural streams, bedrock canyons, and engineering structures. Nevertheless, water flow patterns upstream of horseshoe waterfalls are poorly known and likely differ from the better studied case of a one-dimensional linear step because of flow focusing into the horseshoe. This is a significant knowledge gap because the hydraulics at waterfalls controls sediment transport and bedrock incision, which can compromise the integrity of engineered structures and influence the evolution of river canyons on Earth and Mars. Here we develop new semiempirical theory for the spatial acceleration of water upstream of, and the cumulative discharge into, horseshoe canyons and waterfalls. To this end, we performed 110 numerical experiments by solving the 2-D depth-averaged shallow-water equations for a wide range of flood depths, widths and discharges, and canyon lengths, widths and bed gradients. We show that the upstream, normal flow Froude number is the dominant control on lateral flow focusing and acceleration into the canyon head and that focusing is limited when the flood width is small compared to a cross-stream backwater length scale. In addition, for sheet floods much wider than the canyon, flow focusing into the canyon head leads to reduced discharge (and drying in cases) across the canyon sidewalls, which is especially pronounced for canyons that are much longer than they are wide. Our results provide new expectations for morphodynamic feedbacks between floods and topography, and thus canyon formation.


Item Type:Article
Related URLs:
URLURL TypeDescription
http://dx.doi.org/10.1002/2014JF003412DOIArticle
http://onlinelibrary.wiley.com/doi/10.1002/2014JF003412/abstractPublisherArticle
ORCID:
AuthorORCID
Lapotre, Mathieu G. A.0000-0001-9941-1552
Lamb, Michael P.0000-0002-5701-0504
Additional Information:© 2015 American Geophysical Union. Received 10 DEC 2014; Accepted 11 MAY 2015; Accepted article online 11 MAY 2015; Published online 14 JUL 2015. This work benefited from discussion with Gary Parker, Gareth Davies, and Stephen Roberts. We thank Cailan Haliday for assistance with and testing of the numerical model setup. We also thank three anonymous reviewers for helpful and constructive reviews that improved this paper. Support was provided by the NASA Earth and Space Science Fellowship 12-PLANET12F-0071, NSF Grant EAR-1147381, and NASA Grant NNX13AM83G. All data in the present paper are available upon request to the corresponding author.
Funders:
Funding AgencyGrant Number
NASA Earth and Space Science Fellowship12-PLANET12F-0071
NSFEAR-1147381
NASANNX13AM83G
Subject Keywords:flood hydraulics; waterfall; amphitheater-headed canyon; acceleration factor; bedrock erosion
Record Number:CaltechAUTHORS:20150910-135122139
Persistent URL:http://resolver.caltech.edu/CaltechAUTHORS:20150910-135122139
Official Citation:Lapotre, M. G. A., and M. P. Lamb (2015), Hydraulics of floods upstream of horseshoe canyons and waterfalls. J. Geophys. Res. Earth Surf., 120, 1227–1250. doi: 10.1002/2014JF003412
Usage Policy:No commercial reproduction, distribution, display or performance rights in this work are provided.
ID Code:60174
Collection:CaltechAUTHORS
Deposited By: Tony Diaz
Deposited On:11 Sep 2015 04:17
Last Modified:27 Apr 2017 18:18

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