Articles | Volume 26, issue 5
https://doi.org/10.5194/hess-26-1481-2022
© Author(s) 2022. This work is distributed under the Creative Commons Attribution 4.0 License.
Contrasting changes in hydrological processes of the Volta River basin under global warming
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- Final revised paper (published on 18 Mar 2022)
- Supplement to the final revised paper
- Preprint (discussion started on 27 Oct 2021)
- 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 hess-2021-525', Anonymous Referee #1, 13 Nov 2021
- AC1: 'Reply on RC1', Moctar Dembélé, 14 Jan 2022
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RC2: 'Comment on hess-2021-525', Anonymous Referee #2, 04 Jan 2022
- AC2: 'Reply on RC2', Moctar Dembélé, 18 Jan 2022
Peer review completion
AR – Author's response | RR – Referee report | ED – Editor decision | EF – Editorial file upload
ED: Publish subject to minor revisions (further review by editor) (07 Feb 2022) by Yi He
AR by Moctar Dembélé on behalf of the Authors (10 Feb 2022)
Author's response
Author's tracked changes
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ED: Publish subject to minor revisions (review by editor) (19 Feb 2022) by Yi He
AR by Moctar Dembélé on behalf of the Authors (21 Feb 2022)
Author's response
Author's tracked changes
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ED: Publish subject to technical corrections (22 Feb 2022) by Yi He
AR by Moctar Dembélé on behalf of the Authors (22 Feb 2022)
Manuscript
I enjoyed reading this manuscript. The authors used a distributed model for assessing climate change impacts on different fluxes and discharge output in Volta basin. The ms is quite elaborated and fits well with HESS standards. I only have several concerns regarding “dynamics” and “uncertainty” results presented in the manuscript. Moreover, climate gradient in the basin seems to ruin (dominate) AET patterns censoring vegetation dynamics.
Specific comments:
-Title is very catch but I couldn’t find much on “dynamics” presented in the results except for the Fig5, 13 and 14.
-In addition to Fig13, the readers would be curious to see Lahaa and Blösch (2006) type seasonality figures for regime (a kind of dynamics) changes/shifts in the basin. The seasonality indices could be adopted to low and high flows as done in different other papers below. Event definition is key here for counting them i.e. Q95 and Q5 for low and high flows.
-Seasonality shift is only mentioned for rainfall at line 491 in conclusions but there is room for assessing shifts in high and low flow occurrence (dynamics) and seasonality.
Figures 4-6-9 in Laaha and Blösch (2006) DOI: 10.1002/hyp.6161 are good examples.
Similar applications in climate research:
https://mdpi-res.com/d_attachment/water/water-12-03575/article_deploy/water-12-03575-v3.pdf
https://mdpi-res.com/d_attachment/water/water-11-00925/article_deploy/water-11-00925-v2.pdf
-Fig 11, 12, S38, S49 (AET in particular) are mostly dominated by climate gradient and not showing vegetation dynamics. The authors should find a way to exclude the dominant effect of rainfall using a normalization procedure. A new procedure is proposed in this paper
Example:
https://www.preprints.org/manuscript/202111.0225/v1
However, there must be other methods approaches in the literature for deblurred AET pattern maps by removing climate gradient.
https://www.researchgate.net/publication/338208138_Image_Deblurring_Techniques_-A_Detail_Review
-Line 196: “Uncertainties in the model inputs and outputs are assessed in terms of variability be”
Indicating V2 estimation (or even COV coefficient of variation) as uncertainty assessment is quite ambitious without a systematic uncertainty propagation like in GLUE by Keith Beven.
In short, this vague sentence should be revised as smth like “variability in the model inputs and outputs are assessed using V2 statistics”.