Articles | Volume 26, issue 2
https://doi.org/10.5194/nhess-26-1015-2026
© Author(s) 2026. This work is distributed under the Creative Commons Attribution 4.0 License.
Advancing glacial lake hazard and risk assessment in Bhutan through hydrodynamic flood mapping and exposure analysis
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- Final revised paper (published on 03 Mar 2026)
- Supplement to the final revised paper
- Preprint (discussion started on 14 Jul 2025)
- 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-2025-3206', Anonymous Referee #1, 29 Aug 2025
- AC2: 'Reply on RC1', Sonam Rinzin, 07 Oct 2025
- RC2: 'Comment on egusphere-2025-3206', Adam Emmer, 12 Sep 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) (10 Oct 2025) by Ugur Öztürk
AR by Sonam Rinzin on behalf of the Authors (20 Nov 2025)
Author's response
Author's tracked changes
Manuscript
ED: Referee Nomination & Report Request started (21 Nov 2025) by Ugur Öztürk
RR by Adam Emmer (08 Dec 2025)
RR by Anonymous Referee #1 (19 Dec 2025)
ED: Reconsider after major revisions (further review by editor and referees) (19 Dec 2025) by Ugur Öztürk
AR by Sonam Rinzin on behalf of the Authors (18 Jan 2026)
Author's response
Author's tracked changes
Manuscript
ED: Publish as is (19 Jan 2026) by Ugur Öztürk
AR by Sonam Rinzin on behalf of the Authors (28 Jan 2026)
Manuscript
The study by Rinzin et al. analyses the downstream exposure and vulnerability of infrastructure, buildings and people to glacial lake outburst floods in Bhutan. Their analysis relies on a dataset >200 glacial lakes, a globally available digital elevation model and OSM data. Using HEC-RAS, the authors simulate a scenario for each lake and compare flooding extents, depths and velocity to the locations of the elements at risk.
In general, this is a well-conceived study that leverages hydrodynamic modelling to address some of the weaknesses of previous studies that made quite simplifying assumptions about flood wave propagation and the extent of their impact. However, there are still a few issues with the study which I will outline below. All in all, I recommend major revisions before the manuscript should be published in NHESS.
Major comments:
The parameter choice relies on previously published data (flood volume). However, the choice of parameters does not consider the variability of this data, but rather takes point estimates. For example, the choice of using the median of reported percentages of drainage volume is considered the "most likely flood volume" (L 212). However, if you have a bimodal distribution of partial drainage volumes, then the median is not the most likely flood volume. Thus, it may be useful to not pick out the median scenario, but one that is at the upper end of the distribution, thus giving more weight to extreme scenarios. Same is true for the volume-area relation that may only represents an average of the breadth of possible scenarios. Schwanghart et al. (2016) showed that results of GLOF modelling are not sensitive to uncertainties in the V-A relation for large lakes, but that these uncertainties matter for smaller lakes. I acknowledge that the study already comprises many simulations with quite a heavy computational load. However, it should be at least discussed that the current approach lacks a consideration of the large variability of possible outburst scenarios and that average scenarios may not capture the worst-case scenarios.
A simulation of one or few past GLOFs and comparison of actual with simulated peak discharges would help gaining confidence into the model and its ability to realistically model GLOF dynamics. How can readers evaluate how well your model actually works? This would also enable to tune parameters and eventually study how sensitive the results are to uncertainties in the parameter values.
There are numerous instances were ambiguous or imprecise terms are used. Generally, I think that the terms threat and danger(ous) should be avoided, and that rather terms like hazard (probability of a potentially adverse event happening), exposure (how much are people or infrastructure within reach of a hazardous event), vulnerability (how susceptible are the exposed people or elements) and risk (the combination of the previous, quantitative metrics) should be used as they have a precise and measurable meaning. Threat and danger in turn have a qualitative and subjective meaning. Your work mainly aims to address the exposure of various elements at risk, and you quantify and aggregate the exposure so that it becomes an attribute of each lake. So, to this end, you quantify a lake-specific exposure index.
Minor comments:
41: You state the number of 6907 fatalities, and backpedal later that this number is 80% attributed to a compound event involving the Chorabari outburst. The number of fatalities that can be clearly attributed to the Kedarnath event is probably very uncertain and much lower than those 80%. I would try to tone this more carefully, avoiding reporting numbers with high precision, that actually have a high uncertainty.
49: Provide a definition of danger, in particular if your aim is to quantify it. Rather, as pointed out above, avoid this term entirely.
81: This should be 31%, not 0.31%.
280: How was the HEC-RAS interfaced with? It would be great if you could add a technical description in a paragraph that details how you interfaced with HEC-RAS. I assume that you used the HEC-RAS controller to automate the tasks.
318f: Is it common to take the product of depth and velocity as damage level? Is it useful that the damage level of a water depth of 1 m and velocity of 5 m/s is the same for a water depth of 5 m and a velocity of 1 m/s?
540: It would be helpful to use a stringent and precise terminology here. What is devastating in comparison to damaging? Was the Missoula flood devastating, but not damaging, because no humans were affected (not sure whether this is true)? In simple terms, the risk of GLOFs is mainly determined by the exposed elements at risk, not by their hazard?
594f: I don't think that your approach challenges traditional susceptibility analyses. Rather, your approach may complement them. In contrast to susceptibility studies, your analysis assumes that the outburst probability is homogeneous, thus neglecting any variations in dam stability and lake exposure to avalanches and landslides.
719-721: Considering a risk framework, this is a somewhat trivial statement.
729: Please avoid the high precision of numbers when their estimates are prone to large uncertainties.
Table S1: As the table spans several pages, it would be great to have the header row of this table on each page.
Table S2: Be consistent in the number of digits that you report. Up to 8 digits behind the decimal point suggest an accuracy that you probably don't have in your measurements. When reporting counts (Bridges), use integers.