Articles | Volume 30, issue 1
https://doi.org/10.5194/hess-30-183-2026
https://doi.org/10.5194/hess-30-183-2026
Research article
 | 
14 Jan 2026
Research article |  | 14 Jan 2026

Quantifying uncertainty in flood predictions due to river bathymetry estimation

Martin Nguyen, Matthew D. Wilson, Emily M. Lane, James Brasington, and Rose A. Pearson

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Interactive discussion

Status: closed

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse
  • RC1: 'Comment on hess-2024-356', Anonymous Referee #1, 17 Jan 2025
    • AC1: 'Reply on RC1', martin nguyen, 22 May 2025
  • RC2: 'Comment on hess-2024-356', Anonymous Referee #2, 25 Apr 2025
    • AC2: 'Reply on RC2', martin nguyen, 22 May 2025

Peer review completion

AR – Author's response | RR – Referee report | ED – Editor decision | EF – Editorial file upload
ED: Reconsider after major revisions (further review by editor and referees) (26 May 2025) by Lixin Wang
AR by martin nguyen on behalf of the Authors (26 Jun 2025)  Author's response   Author's tracked changes   Manuscript 
ED: Referee Nomination & Report Request started (27 Jun 2025) by Lixin Wang
RR by Anonymous Referee #1 (14 Jul 2025)
RR by Anonymous Referee #2 (20 Oct 2025)
ED: Publish subject to revisions (further review by editor and referees) (20 Oct 2025) by Lixin Wang
AR by martin nguyen on behalf of the Authors (21 Nov 2025)  Author's response   Author's tracked changes   Manuscript 
ED: Referee Nomination & Report Request started (29 Nov 2025) by Lixin Wang
RR by Anonymous Referee #1 (06 Dec 2025)
ED: Publish as is (25 Dec 2025) by Lixin Wang
AR by martin nguyen on behalf of the Authors (30 Dec 2025)
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Short summary
River depth is crucial in flood modelling, yet often unavailable. Estimation methods can fill this gap but have errors that can affect flood modelling outputs. Our study quantified flood-prediction uncertainty due to these errors. Between Uniform Flow and Conceptual Multivariate Regression formulas, river depths from the former have higher uncertainty than the latter. Among parameters used in these equations, river width corresponds to the largest uncertainty, followed by the flow and slope.
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