Modelling the feedbacks between mass balance, ice flow and debris transport to predict the response to climate change of debris-covered glaciers in the Himalaya

• Published in: Earth and planetary science letters 2015-11, Vol.430, p.427-438
• Main Authors: Rowan, Ann V., Egholm, David L., Quincey, Duncan J., Glasser, Neil F.
• Format: Article
• Language: English
• Subjects: Balancing; Cleaning; Climate change; Debris; Detachment; Everest region; Feedback; glacier dynamics; glacier modelling; Glaciers; Mathematical models; supraglacial debris
• ISSN: 0012-821X; 1385-013X
• DOI: 10.1016/j.epsl.2015.09.004

Many Himalayan glaciers are characterised in their lower reaches by a rock debris layer. This debris insulates the glacier surface from atmospheric warming and complicates the response to climate change compared to glaciers with clean-ice surfaces. Debris-covered glaciers can persist well below the altitude that would be sustainable for clean-ice glaciers, resulting in much longer timescales of mass loss and meltwater production. The properties and evolution of supraglacial debris present a considerable challenge to understanding future glacier change. Existing approaches to predicting variations in glacier volume and meltwater production rely on numerical models that represent the processes governing glaciers with clean-ice surfaces, and yield conflicting results. We developed a numerical model that couples the flow of ice and debris and includes important feedbacks between debris accumulation and glacier mass balance. To investigate the impact of debris transport on the response of a glacier to recent and future climate change, we applied this model to a large debris-covered Himalayan glacier—Khumbu Glacier in Nepal. Our results demonstrate that supraglacial debris prolongs the response of the glacier to warming and causes lowering of the glacier surface in situ, concealing the magnitude of mass loss when compared with estimates based on glacierised area. Since the Little Ice Age, Khumbu Glacier has lost 34% of its volume while its area has reduced by only 6%. We predict a decrease in glacier volume of 8–10% by AD2100, accompanied by dynamic and physical detachment of the debris-covered tongue from the active glacier within the next 150 yr. This detachment will accelerate rates of glacier decay, and similar changes are likely for other debris-covered glaciers in the Himalaya. •Debris-covered glaciers show a differing response to climate change to clean-ice glaciers.•Many glaciers in the Himalaya are debris-covered, particularly in the Everest region.•We present the first dynamic model of debris transport and feedbacks with mass balance.•Debris-covered Khumbu Glacier in Nepal will lose 8–10% volume by AD2100.•The glacier tongue will detach from the active glacier and accelerate glacier decay.