the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Controls on the relatively slow thinning rate of a debris-covered glacier in the Karakoram over the past 20 years: evidence from mass and energy budget modelling of Batura Glacier
Yu Zhu
Ben W. Brock
Lide Tian
Ying Yi
Fuming Xie
Donghui Shangguan
Yiyuan Shen
Abstract. The influence of supraglacial debris cover on glacier dynamics in the Karakoram is noteworthy. However, understanding of how debris cover affects the seasonal and long-term variations in glacier mass balance through alterations in the glacier's energy budget is incomplete. The present study applied an energy-mass balance model coupling heat conduction within debris layers on debris-covered Batura Glacier in Hunza valley, to demonstrate the influence of debris cover on glacial surface energy and mass exchanges during 2000–2020. The mass balance of Batura Glacier is estimated to be -0.262 ± 0.561 m w.e. yr-1, with debris cover reduced 45 % of the negative mass balance. Due to the presence of debris cover, a significant portion of incoming energy is utilized for heating debris, leading to a large energy emission to atmosphere via thermal radiation and turbulent sensible heat. This, in turn, reducing the melt latent heat at the glacier surface. We found that the mass balance exhibits a pronounced arch-shaped structure along the elevation gradient, which primarily attributes to the distribution of debris thickness and the impact of debris cover on the energy budget within various elevation zones. Through a comprehensive analysis of the energy transfer within each debris layer, we have demonstrated that the primary impact of debris cover lies in its ability to modify the energy flux reaching the surface of the glacier. Thicker debris cover results in a smaller temperature contrast between debris layers and the ice-contact zone, consequently reducing heat conduction. Over the past two decades, Batura Glacier has maintained a relatively small negative mass balance, owing to the protective effect of debris cover. The glacier exhibits a tendency towards a smaller negative mass balance, with diminishing dominance of ablation in areas with thin debris cover and debris-free parts of the ablation area.
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Yu Zhu et al.
Status: open (until 01 Jan 2024)
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RC1: 'Comment on hess-2023-238', Anonymous Referee #1, 15 Nov 2023
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The presence of supraglacial debris significantly influences the energy exchange both entering and leaving the glacier surface, thereby impacting glacier mass balance, movement, and associated glacio-hydrological processes. Despite substantial efforts in on-site observations and mathematical modeling, the specific mechanisms and extent of debris effects on glaciers remain unresolved. This study focuses on the Batura Glacier in the Hunza River Basin, offering a quantitative, comprehensive understanding of how debris cover affects energy and mass balance, with potential implications for glaciers under similar conditions. The contribution of this research is anticipated to attract interest from the scientific communities engaged in glaciology and hydrology.
General Comments:
1. The effects of debris cover on energy and mass balance are intricately linked to local climate, topography, and the characteristics of the debris and ice body. Consideration of factors such as coverage, thickness, constituents, and heat properties of debris is pivotal when discussing their impact. Providing detailed information on the debris cover, including a spatial distribution map, is recommended.
2. The study employs the physically based energy balance model COSIPY v1.3 and the debris cover model by Reid and Brock (2010). A concise and meaningful description of these models, along with clarification on the simulation of heat transfer within the ice body, model integration, and boundary condition setup at interfaces (snow-debris, debris-ice) is essential. The manuscript should include a graphic illustration depicting the integration of models and energy transfer within the snow-debris-ice body system.
3. Clarify whether the snow and debris are delineated into different layers vertically during simulations and elaborate on the methodology.
4. The models are parameterized using observation data at AWS(s). Specify the target functions during parameterization, evaluate the rationality of final parameters, and explain the process of extending these parameters to simulate the entire Batura Glacier.
5. Present the results of heat exchange at the debris – ice interface and discuss the debris – ice interactions at typical cross-sections along the glacier.
6. In the Conclusion section, emphasize how and to what extent the unconsidered factors that may cause uncertainties in the results could influence the outcomes. Address these aspects more explicitly in the Results and Discussion section.
7. Rearrange section 4.1, presenting "4.1.2 energy budgets" before "4.1.1 mass balance history" for better coherence.
8. Given that the debris cover controls the relatively slow thinning of the glacier, consider revising the title to a more concise version such as "Debris Cover Effects on Energy and Mass Balance of Batura Glacier in the Karakoram."
Specific Comments:
1. Ensure that figures are appropriately placed closer to their first citation and that all figures include clear labels, units, and legends for improved readability.
2. Follow customary practices where symbol descriptions closely follow mathematical formulas, especially for complex equations requiring detailed symbol explanations. Ensure completeness in symbol descriptions for all mathematical formulas.
Citation: https://doi.org/10.5194/hess-2023-238-RC1
Yu Zhu et al.
Yu Zhu et al.
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