REVIEW 4 major objections 6 minor 68 references
Effect of Discharge on the Nonlinear Bar Growth: A Flume Experiment
T0 review · 4 major / 6 minor · reviewed 2026-08-08 · deepseek-v4-flash
Pith's one-line read This paper reports flume experiments that, for the first time, continuously track alternate-bar growth without stopping the flow, and compares the measured growth rates with weakly nonlinear theory.
desk verdict Solid new bar-growth dataset with a plausible qualitative trend; the quantitative comparison to theory needs error bars and pre-specified exclusions before the headline claim is trusted. read the letter →
The pith
A machine-rendered reading of the paper's core claim, the machinery that carries it, and where it could break.
The reading
What carries the argument
The central device is Stream Tomography, a laser-sheet and camera cart that maps the bed at one-minute intervals and one-centimeter-squared resolution while the flow continues, supplying complete time series of bar height $H_{\mathrm{MB}}(t)$. These series are fitted with the general solution of the Landau equation, which yields the growth rate $\Omega_{H_{\mathrm{MB}}}$ and equilibrium height $H_{\mathrm{MB}e}$ as empirical coefficients, with time made dimensionless using the Exner bedload timescale $t^* = t\,q_{s0}/((1-p)h_0 B/2)$. The hydraulic interpretation rests on fixed-bed, depth-averaged flow simulations over the measured topography, from which the authors compute the flow-deflection ratio $|v|/u$ and the area where the Shields stress falls below the critical value for sediment motion.
What would settle it
Recompute the bar-height derivative directly from the raw Stream Tomography time series and test whether $(dH_{\mathrm{MB}}/dt)/H_{\mathrm{MB}}$ is a linear function of $(H_{\mathrm{MB}}/H_{\mathrm{MB}e})^2$. A systematic departure from that line — particularly during the fast-growth phase, where the fit is least good — would show that the Landau equation is only an approximation and that the reported $\Omega_{H_{\mathrm{MB}}}$ values cannot be identified with the theoretical linear growth rate. The bar-celerity mechanism could be checked independently by measuring sediment flux directly and comparing it with the relation $C = q_s / (2(1-p)Z)$ used in the paper.
Extended reading notes
Core claim
On a dimensionless bedload timescale, alternate-bar height in the flume grows faster and to a higher equilibrium value when discharge is lower. The full growth curves, captured without stopping the flow, are well described by the Landau equation $$\frac{dH_{\mathrm{MB}}}{dt} = \Omega_{H_{\mathrm{MB}}} H_{\mathrm{MB}} \left(1 - \left(\frac{H_{\mathrm{MB}}}{H_{\mathrm{MB}e}}\right)^2\right),$$ and the fitted dimensionless growth rate $\Omega_{H_{\mathrm{MB}}}$ increases as discharge decreases, but its sensitivity is weaker than the maximum linear growth rate of the single alternate-bar mode ($m=1$) predicted by linear stability theory; the discrepancy grows at lower discharge. Fixed-bed flow calculations over the measured topography explain the trend: at low discharge the bar is tall relative to flow depth, flow deflection is stronger, non-transport zones spread downstream of depositional areas, bar migration slows, and flow and sediment transport concentrate in the scour zone, deepening the pools that set bar height.
Load-bearing premise
The load-bearing premise is that bar height $H_{\mathrm{MB}}(t)$ — a composite quantity made of many Fourier modes — evolves according to the same Landau equation as the amplitude $\alpha_{11}$ of a single alternate-bar mode; the paper itself notes there is no theoretical guarantee of this, and if the true evolution is not Landau-type, the fitted growth rates are not the quantities being compared with stability theory.
Editorial extensions
If this is right
- Lower discharge on a bedload-based timescale makes alternate bars grow faster and reach a larger equilibrium height, so a sustained discharge reduction should make bars taller and less mobile.
- The measured growth-rate-versus-discharge curve gives stability theories a quantitative target: they must reproduce a weaker-than-linear sensitivity, especially at low discharge.
- Bar-height growth in these runs is dominated by deepening scour rather than rising deposition, so monitoring the minimum bed elevation alone can track height development.
- Flow deflection, non-transport zones, and bar celerity respond together with bar height, meaning bar development is a self-reinforcing feedback rather than a one-way response to discharge.
Reading between the lines
- Inference: the fitted $\Omega_{H_{\mathrm{MB}}}$ values could be used to calibrate the intermodal coupling coefficients in the two-mode amplitude equations the paper sketches, turning the observed growth of $\alpha_{20}$ into a quantitative correction to the single-mode theory.
- Inference: if linear theory systematically overshoots the discharge sensitivity of bar growth, flood-frequency projections built on single-mode growth rates may overstate future bar-height change; checking this would require matching long bed-elevation records to discharge histories in real rivers.
- Inference: the mechanism implies a testable crossover — the regime of bimodal flow deflection, large non-transport zones, and suppressed migration should begin near a particular bar height-to-depth ratio, which a future experiment could isolate by varying discharge at fixed slope.
Editorial analysis
A structured set of objections, weighed in public.
Referee Report
Summary. The paper reports a laboratory flume study of alternate-bar development under four discharges and four channel slopes (16 conditions, at least five replicates each), using the non-intrusive Stream Tomography technique to measure bed topography continuously without interrupting flow. Bar height H_MB is defined as the max-minus-min bed elevation within a tracked half-wavelength, and its temporal evolution is fitted to the general solution of the Landau equation (Eq. 6) to extract a growth rate Omega_HMB and equilibrium height H_MBe. The dimensionless growth rate is then compared against the linear stability theory of Colombini et al. (1987) for the single alternate-bar mode alpha_11, using two sediment-transport formulas (Meyer-Peter and Mueller, Parker). The central empirical claim is that the growth rate of bar height increases as discharge decreases on a bedload-based timescale, but its sensitivity to discharge is weaker than the theoretical sensitivity of the linear growth rate, with the discrepancy growing at lower discharge. Fixed-bed Nays2D simulations over measured bed topographies are used to propose a mechanism: lower discharge produces larger height-to-depth ratios, stronger flow deflection, expanded non-sediment-transport zones, reduced bar migration, and concentration of transport in scour zones, promoting bar-height growth. Case 16 and some replicates are excluded from the analysis on criteria that are only partly specified in advance.
Significance. If upheld, the paper would provide the first continuous experimental estimates of the nonlinear growth coefficient of the Landau equation for alternate bars and a benchmark for bar stability theories, which is a meaningful contribution to fluvial geomorphology. The study has notable strengths: a multi-replicate design that addresses inherent variability in bar formation; a non-intrusive measurement technique that avoids flow interruption; direct data availability via a Zenodo dataset; and an explicit statement of the main modeling assumption, including its caveat. The hydraulic calculations over measured bed topography add a physically plausible mechanistic interpretation. However, the central claim depends on the unvalidated substitution of bar height H_MB for the single-mode amplitude alpha_11 in the Landau equation, and the headline discharge-sensitivity comparison lacks confidence intervals or significance testing. These issues are load-bearing for the main conclusion and require additional analysis before the result can be considered established.
major comments (4)
- [Section 3.3.1, Eq. (5)] The identification of the measured bar height H_MB with the single-mode amplitude alpha_11 in Eq. (5) is the load-bearing step of the paper. The authors themselves state that 'there is no theoretical guarantee that bar height follows a Landau equation.' H_MB is a composite quantity defined over a half-wavelength and contains contributions from alpha_20 and other modes; Appendix B reports alpha_20/alpha_11 up to about 0.8. Consequently, the fitted Omega_HMB is a lumped, model-dependent growth rate, not the linear growth rate Omega_11 of the most amplified single bar mode. Figure 8 then compares the discharge sensitivity of this fitted quantity with the theoretical sensitivity of Omega_11. If a different saturation form, or no Landau form, describes the data, the fitted Omega_HMB and the power-law exponent a would change, and the central claim about weaker-than-linear sensitivity could weaken or reverse. The paper should provide a sensitivity analysis with alternative sigmoidal forms (e.g., logistic or Gompertz), or an explicit derivation of how modal superposition biases the fitted growth rate, to show that the headline conclusion does not rely solely on the Landau functional form.
- [Section 3.3.2, Figure 8] The headline claim that the experimental growth rate is 'less sensitive' to discharge than the theoretical prediction is based on power-law fits y = b Q^a plotted in Figure 8, but no confidence intervals, standard errors, or significance tests are reported for the exponent a or for the comparison against the theoretical exponents. With at least three replicates per condition after screening, a bootstrap or mixed-effects analysis is feasible and would directly address whether the observed weaker sensitivity is statistically robust across slopes. As written, the visual separation in Figure 8 is not quantified, and the statement that the discrepancy 'becomes more pronounced at lower discharge' also lacks a formal test. These statistical gaps undermine the paper's central quantitative conclusion.
- [Section 3, exclusions of Case 16 and replicates] The exclusion of Case 16 (Q = 1.7 L/s, I = 1/200) and of replicates with 'substantially lower reproducibility than the others' is partly post-hoc and may bias the discharge-sensitivity comparison. Case 16 is precisely the lowest-discharge, lowest-slope condition, the regime where the discrepancy with theory is largest, so excluding it could strengthen the appearance of a monotonic discharge trend. The authors should either justify exclusions with a pre-specified protocol, or report how the Figure 8 results change when Case 16 and the excluded replicates are included. Without this, the robustness of the inferred power-law exponents to data-selection choices remains unclear.
- [Appendix A1] The goodness of fit R^2 > 0.90 (and about 0.75 in the least favorable case) is cited as evidence that the Landau equation adequately represents bar-height evolution, but this does not validate the functional form: many sigmoidal curves fit such time series equally well. The statistical screening that removes coefficients with p > 0.05 assesses coefficient reliability, not model adequacy. A residual analysis, a comparison with alternative growth-and-saturation models, or a test of the implied relationship between growth rate and current height (e.g., dH_MB/dt divided by H_MB versus H_MB^2) would provide much stronger support for the use of Eq. (5).
minor comments (6)
- [Section 3.3.1] There is an internal equation-numbering inconsistency: the text says 'Equation (6)' when referring to the Landau equation, but Eq. (5) is the Landau equation and Eq. (6) is its general solution; please correct the cross-references.
- [Table 1 and Figure 3] The caption of Figure 3 does not note that panel (o) is absent for I = 1/200 due to the exclusion of Case 16; please state this in the caption or figure layout for clarity.
- [Section 2.1] The critical discharge Q_c appearing in Table 1 is said to be 'calculated by the method described later,' but the method is not described in Section 2.1; please provide the formula or a forward reference to Section 3.3.2 where the stability analysis is presented.
- [Figure 8, legend] The legend entries '0.3' and '0.7' for the theoretical curves are not explained in the caption; they should be identified as the r values (transverse bedload direction coefficient) used in the stability analysis.
- [Section 5.1.2, Eq. (11)] The piecewise expression for H_MB/h_0 in Eq. (11) is introduced without derivation or definition of the symbols beyond the preceding amplitudes; please clarify how this composite expression arises from the two-mode evolution equations (9) and (10).
- [Various] Several typographical issues need correction: 'manuscript submitted toJGR' appears without the intended spacing; 'v/upales' in the Figure 9 caption should read 'v/u panels'; and 'T able 1' heading contains an extra space.
Circularity Check
No significant circularity: the empirical Landau-fit growth rates are compared against an external linear-stability benchmark, and self-citations concern the measurement technique rather than the target result.
full rationale
The paper's central derivation is the fit of Eq. (6), the general solution of the Landau equation, to measured bar-height time series, yielding the empirical growth rate Omega_HMB, followed by a comparison of Omega_HMB with the linear-theory growth rate Omega_11 computed from Colombini et al. (1987). The fitted quantity is not defined in terms of the theoretical quantity; the two are obtained independently, so the reported weaker sensitivity to discharge is an empirical outcome that could in principle have gone the other way. The paper explicitly flags the substitution of H_MB for alpha_11 as an approximation, stating 'Because bars are a superposition of multiple Fourier components, there is no theoretical guarantee that bar height follows a Landau equation,' and it provides goodness-of-fit diagnostics in Appendix A1. That is an acknowledged model assumption, not a circular definition or a fitted input renamed as a prediction. The self-citations (Moteki et al. 2022; Ishihara and Yasuda 2022; Moteki et al. 2023; Seki et al. 2023) support the Stream Tomography measurement technique and the perturbation design, not the growth-rate conclusion, and the main comparison uses external theory and empirical benchmarks (Colombini et al. 1987; S. Ikeda 1984). The non-sediment-transport-zone analysis is a quantitative diagnostic based on the criterion tau* < tau*_c; while lower base Shields numbers make the threshold easier to cross, the reported spatial patterns and their dependence on bar height are computed from measured bed topography rather than imposed by the claim. No equation in the paper reduces to its own input by construction, and no parameter fitted to a subset of data is subsequently presented as a prediction of that same subset. Therefore the honest finding is no significant circularity.
Assumptions & free parameters
free parameters (2)
- r (bedload transverse transport direction coefficient) =
0.3-0.7 (swept)
- Landau coefficients Omega_HMB, H_MBe, H_MB0 per replicate =
Per-condition fitted values (Appendix A1)
assumptions (6)
- ad hoc to paper Bar height H_MB(t) follows the Landau equation (Eq. 5) with H_MB substituted for the single-mode amplitude alpha_11.
- domain assumption The Exner-based dimensionless time t* (Eq. 1) with the Meyer-Peter-Muller bedload formula is the appropriate common clock for comparing growth rates across discharges.
- domain assumption The maximum linear growth rate of the single (m,n)=(1,1) mode from Colombini-type stability analysis is the correct benchmark for the growth rate of composite bar height.
- domain assumption Bar-height growth in these experiments is governed primarily by progressive scour rather than deposition.
- domain assumption Nays2D depth-averaged fixed-bed simulations with the measured bed prescribed and Manning-Strickler roughness reproduce the flow deflection and shear-stress distributions relevant to bar growth.
- domain assumption Non-sediment-transport zones are identified by the criterion tau* < tau*c = 0.034.
Cite this review
Pith. "Pith review of Effect of Discharge on the Nonlinear Bar Growth: A Flume Experiment." pith.science (2026). https://pith.science/paper/WYKR4OXT
@misc{pith2026260805593,
author = {Pith},
title = {Pith review of: Effect of Discharge on the Nonlinear Bar Growth: A Flume Experiment},
year = {2026},
howpublished = {\url{https://pith.science/paper/WYKR4OXT}},
note = {Machine review of arXiv:2608.05593}
}
read the original abstract
Alternate bars are ubiquitous bedforms in alluvial rivers, and excessive bar-height growth can increase flood risk and disrupt ecosystems. Predicting bar-height variability requires quantifying the dependence of bar growth rate on water discharge, yet this has rarely been achieved because conventional flume measurements interrupt the flow and cannot continuously capture bar evolution. Here we conducted laboratory experiments under four discharges and four channel slopes (16 conditions) and continuously mapped bed topography using Stream Tomography, a nonintrusive, flow-through measurement technique. Bar height exhibits sigmoidal growth and is well described by the Landau equation, allowing robust estimation of the growth rate and equilibrium height. The inferred dimensionless growth rate tends to increase as discharge decreases, but its sensitivity is weaker than that predicted by stability theory for a single alternate-bar mode. This discrepancy becomes more pronounced at lower discharge, indicating limitations of linearization and the influence of interactions among multiple bar modes. Furthermore, numerical flow simulations over the measured bed topography reveal that, during bar development, lower-discharge conditions produce a relatively larger bar height-to-depth ratio, making the flow more prone to deflection. In such cases, sediment transport is restricted downstream of depositional areas, thereby limiting bar migration. Consequently, flow and sediment transport become concentrated in the scour zones, enhancing local scour and promoting the growth of bar height. These results provide benchmark constraints for bar stability theories and help improve predictions of how bar height responds to changes in discharge.
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Works this paper leans on
- [1]
- [2]
-
[3]
Visconti, F. and Camporeale, C. and Ridolfi, L. , title =. J. Geophys. Res. , volume =. 2010 , doi =
work page 2010
-
[4]
Nagata, T. and Watanabe, Y. and Yasuda, H. and Ito, A. , title =. Earth Surf. Dynam. , volume =. 2014 , doi =
work page 2014
-
[5]
Inoue, T. and Hiramatsu, Y. and Johnson, J. P. L. and Dempo, J. and Mishra, J. , title =. J. Geophys. Res. Earth Surf. , volume =. 2025 , doi =
work page 2025
- [6]
-
[7]
Richard Hauer and Harvey Locke and Victoria J
F. Richard Hauer and Harvey Locke and Victoria J. Dreitz and Mark Hebblewhite and Winsor H. Lowe and Clint C. Muhlfeld and Cara R. Nelson and Michael F. Proctor and Stewart B. Rood , title =. Sci. Adv. , volume =. 2016 , doi =
work page 2016
-
[8]
Hu, Y. and Deng, J. and Li, D. and Lu, X. and Zhou, J. and Wang, C. and Li, Y. , title =. Geophys. Res. Lett. , volume =. 2024 , doi =
work page 2024
Show all 68 references
-
[9]
Impact of river regulation on gravel bar decline and vegetation expansion over recent decades , journal =
Holu. Impact of river regulation on gravel bar decline and vegetation expansion over recent decades , journal =. 2025 , doi =
2025
-
[10]
and Mahendran, R
Hirabayashi, Y. and Mahendran, R. and Koirala, S. and Konoshima, L. and Yamazaki, D. and Watanabe, S. and Kim, H. and Kanae, S. , title =. Nature Climate Change , volume =. 2013 , doi =
2013
-
[11]
Arnell, N. W. and Gosling, S. N. , title =. Climate Change , volume =. 2016 , doi =
2016
-
[12]
and Hirabayashi, Y
Tanoue, M. and Hirabayashi, Y. and Ikeuchi, H. , title =. Sci. Rep. , volume =. 2016 , doi =
2016
-
[13]
Changing climate both increases and decreases European river floods , journal =
Bl. Changing climate both increases and decreases European river floods , journal =. 2019 , doi =
2019
-
[14]
and Villarini, G
Slater, L. and Villarini, G. and Archfield, S. and Faulkner, D. and Lamb, R. and Khouakhi, A. and Yin, J. , title =. Geophys. Res. Lett. , volume =. 2021 , doi =
2021
-
[15]
and Welber, M
Redolfi, M. and Welber, M. and Carlin, M. and Tubino, M. and Bertoldi, W. , title =. Earth Surf. Dynam. , volume =. 2020 , doi =
2020
-
[16]
and Morgan, J
Nelson, P. and Morgan, J. , title =. Geomorphology , volume =. 2018 , doi =
2018
-
[17]
and Kishi, T
Kuroki, M. and Kishi, T. , title =. Proceedings of the Japan Society of Civil Engineers (in Japanese) , volume =. 1984 , doi =
1984
-
[18]
and Seminara, G
Colombini, M. and Seminara, G. and Tubino, M. , title =. J. Fluid Mech. , volume =. 1987 , doi =
1987
-
[19]
, title =
Redolfi, M. , title =. Water Resour. Res. , volume =. 2021 , doi =
2021
-
[20]
and Tubino, M
Lanzoni, S. and Tubino, M. , title =. J. Fluid Mech. , volume =. 1999 , doi =
1999
-
[21]
and Repetto, R
Tubino, M. and Repetto, R. and Zolezzi, G. , title =. J. Hydraul. Res. , volume =. 1999 , doi =
1999
-
[22]
and Shimizu, Y
Iwasaki, T. and Shimizu, Y. and Kimura, I. , title =. Adv. Water Resour. , volume =. 2016 , doi =
2016
-
[23]
Stability analysis of ecomorphodynamic equations , journal =
B. Stability analysis of ecomorphodynamic equations , journal =. 2016 , doi =
2016
-
[24]
, title =
Kinoshita, R. , title =. Bureau of Resources, Science and Technology Agency, Research Material (in Japanese) , volume =. 1961 , doi =
1961
-
[25]
and Muramoto, Y
Fujita, Y. and Muramoto, Y. , title =. Bulletin of the Disaster Prevention Research Institute , volume =. 1982 , doi =
1982
-
[26]
and Muramoto, Y
Fujita, Y. and Muramoto, Y. , title =. Bulletin of the Disaster Prevention Research Institute , volume =. 1985 , doi =
1985
-
[27]
, title =
Ikeda, H. , title =. Environmental Research Center Papers, The University of Tsukuba , volume =. 1983 , doi =
1983
-
[28]
Jaeggi, M. N. R. , title =. J. Hydraul. Eng. , volume =. 1984 , doi =
1984
-
[29]
, title =
Ikeda, S. , title =. J. Hydraul. Eng. , volume =. 1984 , doi =
1984
-
[30]
and da Silva, A
Cheng, Y. and da Silva, A. M. F , title =. J. Hydraul. Eng. , volume =. 2019 , doi =
2019
-
[31]
and Doelman, A
Schielen, R. and Doelman, A. and Swart, H. E. , title =. J. Fluid Mech. , volume =. 1993 , doi =
1993
-
[32]
, title =
Tubino, M. , title =. Water Resour. Res. , volume =. 1991 , doi =
1991
-
[33]
, title =
Hall, P. , title =. J. Fluid Mech. , volume =. 2004 , doi =
2004
-
[34]
Welford, M. R. , title =. Earth Surf. Process. Landf. , volume =. 1994 , doi =
1994
-
[35]
Bertagni, M. B. and Camporeale, C. , title =. Water Resour. Res. , volume =. 2018 , doi =
2018
-
[36]
Ali, S. Z. and Dey, S. and Mahato, R. K. , title =. Proc. R. Soc. A , volume =. 2021 , doi =
2021
-
[37]
and Redolfi, M
Carlin, M. and Redolfi, M. and Tubino, M. , title =. Water Resour. Res. , volume =. 2021 , doi =
2021
-
[38]
and Takatsu, S
Izumi, N. and Takatsu, S. and Kawamura, S. , title =. Journal of Japan Society of Civil Engineers, Ser. A2 (Applied Mechanics) (in Japanese) , volume =. 2021 , doi =
2021
-
[39]
and Kawamura, S
Izumi, N. and Kawamura, S. , title =. Journal of Japan Society of Civil Engineers, Ser. B1 (Hydraulic Engineering) (in Japanese) , volume =. 2022 , doi =
2022
-
[40]
and Yamaoka, I
Hasegawa, K. and Yamaoka, I. , title =. Proceedings of the Japanese Conference on Hydraulic (in Japanese) , volume =. 1982 , doi =
1982
-
[41]
Garcia, M. and Ni. Dynamics of sediment bars in straight and meandering channels: experiments on the resonance phenomenon , journal =. 1993 , doi =
1993
-
[42]
and Carlin, M
Redolfi, M. and Carlin, M. and Tubino, M. , title =. Geophys. Res. Lett. , volume =. 2023 , doi =
2023
-
[43]
and Iwasaki, T
Inoue, T. and Iwasaki, T. and Sumner, T. and Hiramatsu, Y. and Ozeki, T. and Sasaki, S. and Tomino, T. and Kido, R. , title =. Journal of Japan Society of Civil Engineers, Special Issue (Hydraulic Engineering) (in Japanese) , volume =. 2024 , doi =
2024
-
[44]
and Murai, T
Moteki, D. and Murai, T. and Hoshino, T. and Yasuda, H. and Muramatsu, S. and Hayasaka, K. , title =. Phys. Fluids , volume =. 2022 , doi =
2022
-
[45]
, title =
Ishihara, M and Yasuda, H. , title =. J. Geophys. Res. Earth Surf. , volume =. 2022 , doi =
2022
-
[46]
and Seki, S
Moteki, D. and Seki, S. and Muramatsu, S. and Hayasaka, K. and Yasuda, H. , title =. Phys. Fluids , volume =. 2023 , doi =
2023
-
[47]
and Moteki, D
Seki, S. and Moteki, D. and Yasuda, H. , title =. Phys. Fluids , volume =. 2023 , doi =
2023
-
[48]
, title =
Iwagaki, Y. , title =. Transactions of the Japan Society of Civil Engineers (in Japanese) , volume =. 1956 , doi =
1956
-
[49]
Meyer-Peter, E. and M. Formulas for Bed-Load transport , journal =
-
[50]
Nelson, J. M. and Shimizu, Y. and Abe, T. and Asahi, K. and Gamoue, M. and Inoue, T. and Iwasaki, T. and Kakinuma, T. and Kawamura, S. and Kimura, I. and Kyuka, T. and McDonald, R. R. and Nabi, M. and Nakatsugawa, M. and Sim. The international river interface cooperative: Publ...
2016
-
[51]
and Nelson, J
Shimizu, Y. and Nelson, J. and Ferrel, K. A. and Asahi, K. and Giri, S. and Inoue, T. and Iwasaki, T. and Jang, C-L. and Kang, T. and Kimura, I. and Kyuka, T. and Mishara, T. and Nabi, M. and Patsinghasanee, S. and Yamaguchi, S. , title =. Earth Surf. Process. Landf. , volume ...
2019
-
[52]
and Desta, F
Crosato, A. and Desta, F. B. and Cornelisse, J. and Schuurman, F. and Uijttewaal, W. S. J. , title =. Water Resour. Res. , volume =. 2012 , doi =
2012
-
[53]
and Muramoto, Y
Fujita, Y. and Muramoto, Y. , title =. Disaster Prevention Research Institute annuals (in Japanese) , volume =. 1975 , doi =
1975
-
[54]
, title =
Parker, G. , title =. J. Fluid Mech. , volume =. 1978 , doi =
1978
-
[55]
and Hansen, E
Engelund, F. and Hansen, E. , title =. Technical University of Denmark Ostervoldgade , pages =
-
[56]
and Yamasaka, Y
Fukuoka, S. and Yamasaka, Y. , title =. Proceedings of the Japan Society of Civil Engineers (in Japanese) , volume =. 1985 , doi =
1985
-
[57]
and Yamasaka, Y
Fukuoka, S. and Yamasaka, Y. and Shimizu, Y. , title =. Proceedings of the Japan Society of Civil Engineers (in Japanese) , volume =. 1985 , doi =
1985
-
[58]
and Ishii, C
Kuroki, M. and Ishii, C. and Itakura, T. , title =. Proceedings of Hydraulic Engineering (in Japanese) , volume =. 1992 , doi =
1992
-
[59]
and Pornprommin, A
Izumi, N. and Pornprommin, A. , title =. Proceedings of the Japan Society of Civil Engineers (in Japanese) , volume =. 2002 , doi =
2002
-
[60]
and Kuwamura, T
Watanabe, Y. and Kuwamura, T. , title =. Proceedings of Hydraulic Engineering (in Japanese) , volume =. 2005 , doi =
2005
-
[61]
, title =
Watanabe, Y. , title =. Proceedings of Hydraulic Engineering (in Japanese) , volume =. 2006 , doi =
2006
-
[62]
Lisle, T. E. and Ikeda, H. and Iseya, F. , title =. Earth Surf. Process. Landf. , volume =. 1991 , doi =
1991
-
[63]
, title =
Seki, S. , title =. Zenodo , year =
-
[64]
and Devineni, N
Najibi, N. and Devineni, N. , title =. Earth Syst. Dynam. , volume =. 2018 , doi =
2018
-
[65]
and Rinaldi, M
Belletti, B. and Rinaldi, M. and Buijse, A. D. and Gurnell, A. M. and Mosselman, E. , title =. Environ. Earth Sci. , volume =. 2015 , doi =
2015
-
[66]
Bank erosion processes measured with UAV-SfM along complex banklines of a straight mid-sized river reach , journal =
Dur. Bank erosion processes measured with UAV-SfM along complex banklines of a straight mid-sized river reach , journal =. 2018 , doi =
2018
-
[67]
and Gong, Z
Zhao, K. and Gong, Z. and Zhang, K. and Wang, K. and Jin, C. and Zhou, Z. and Xu, F. and Coco, G. , title =. J. Geophys. Res. Earth Surf. , volume =. 2020 , doi =
2020
-
[68]
Das, V. K. and Debnath, K. , title =. J. Hydrol. , volume =. 2025 , doi =
2025
Reviewed August 8, 2026 · model on record in the stance chip above.
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