Articles | Volume 30, issue 8
https://doi.org/10.5194/hess-30-2493-2026
© Author(s) 2026. This work is distributed under the Creative Commons Attribution 4.0 License.
What can hydrological modelling gain from spatially explicit parameterization and multi-gauge calibration?
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- Final revised paper (published on 29 Apr 2026)
- Supplement to the final revised paper
- Preprint (discussion started on 02 Feb 2026)
- Supplement to the preprint
Interactive discussion
Status: closed
Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor
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RC1: 'Comment on egusphere-2025-6543', Anonymous Referee #1, 27 Feb 2026
- AC1: 'Reply on RC1', Xudong Zheng, 01 Mar 2026
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RC2: 'Comment on egusphere-2025-6543', Anonymous Referee #2, 17 Mar 2026
- AC2: 'Reply on RC2', Xudong Zheng, 18 Mar 2026
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) (24 Mar 2026) by Hongkai Gao
AR by Xudong Zheng on behalf of the Authors (30 Mar 2026)
Author's response
Author's tracked changes
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ED: Referee Nomination & Report Request started (02 Apr 2026) by Hongkai Gao
RR by Brandi Gaertner (10 Apr 2026)
RR by Anonymous Referee #1 (12 Apr 2026)
ED: Publish subject to technical corrections (16 Apr 2026) by Hongkai Gao
AR by Xudong Zheng on behalf of the Authors (18 Apr 2026)
Author's response
Manuscript
The manuscript presents a timely and highly relevant investigation into the combined effects of spatially explicit parameterization and multi-gauge calibration on hydrological modeling. The paper is well-written, logically structured, and provides a meaningful steppingstone for the advancement of modern Model-Data Infusion frameworks. However, there are several issues needed to be addressed before publication.
Specific comments:
1. In the parameter calibration, the authors did not consider three key VIC parameters that are commonly calibrated, namely Ds, Ws, and Dm. Although Gou et al. (2020) is cited in the manuscript, that study does not provide sensitivity analysis results for the specific basin investigated here. Including these parameters in the calibration process could potentially lead to different results. Therefore, the authors are encouraged to provide sensitivity analysis results for the study basin to justify the exclusion of these parameters. Otherwise, I believe that Ds, Ws, and Dm should be incorporated into the calibration.
2. The use of MPR is indeed an effective approach for deriving distributed parameters; however, one of its key limitations lies in the uncertainty associated with the transfer functions. Previous studies have shown that different transfer functions can lead to substantially different calibration results. For example, Gou et al. (2021) adopted transfer functions for D1–D3 that differ from those used in this study. It remains unclear whether such differences could lead to different conclusions. The manuscript currently lacks analysis and discussion on this issue, which should be addressed to strengthen the robustness of the study.
Gou, Jiaojiao, et al. "CNRD v1. 0: a high-quality natural runoff dataset for hydrological and climate studies in China." Bulletin of the American Meteorological Society 102.5 (2021): E929-E947.
3. The manuscript currently lacks sufficient statistical validation of the calibration experiments. Without statistical evaluation, it is difficult to determine whether the reported improvements reflect meaningful advancements or merely small fluctuations. For instance, an KGE difference between 0.715 and 0.716 in Table 6 is not necessarily meaningful without significance testing. The authors are encouraged to incorporate appropriate statistical tests, such as the Wilcoxon signed-rank test or paired t-tests for comparisons. In addition, reporting the standard deviation (you only showed ensemble mean) across ensemble runs would substantially strengthen the credibility of the results.
4. The description of the two-step mechanism for reconciling soil data with the VIC three-layer (VIC-3L) vertical structure is confusing. Since Table 2 already presents the transfer functions for D1–D3, it is unclear what additional role this two-step procedure plays. Because this component underpins the subsequent analysis, a more detailed and transparent explanation is essential.
5. The authors designed eight calibration experiments; however, the current numerical labeling makes it difficult for readers to remember the specific configurations during subsequent discussion. It is recommended that the authors adopt clearer and more descriptive naming conventions to distinguish the different experiments, which would improve readability and interpretability.
6. When applying the NSGA-II algorithm for multi-objective optimization, the implementation details are not sufficiently described. Given that the study basin includes five gauging stations, does this imply that five separate objectives were defined for calibration? The authors should clearly specify how the objective functions were formulated and aggregated, and how the multi-objective framework was structured in practice.
7. The authors should include, in Table 5, the ranges for all parameters to be optimized. Providing the parameter bounds would improve transparency and allow readers to better assess the robustness and reproducibility of the calibration procedure.
8. Although the authors provided a zoomed-in view in Figure 5, the differences remain unclear. From my perspective, the four schemes perform almost identically in the high-flow segment.