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Role of supraglacial ponds in the ablation process of a debris-covered glacier in the Nepal Himalayas

2000; International Association of Hydrological Sciences; Linguagem: Inglês

0144-7815

Akiko Sakai, Nozomu Takeuchi, Koji Fujita, Masayoshi Nakawo,

Climate change and permafrost

There are many supraglacial ponds on debris-covered glaciers in the Nepal Himalayas. The heat absorbed at the surface of a pond was estimated from heat budget observations on the Lirung Glacier in Langtang Valley, Nepal. The results indicated an average heat absorption of 170 W m -2 during the summer monsoon season. This rate is about 7 times the average for the whole debris-covered zone. Analysis of the heat budget for a pond suggests that at least half of the heat absorbed at a pond surface is released with the water outflow from the pond, indicating that the water warmed in the pond enlarges the englacial conduit that drains water from the pond and produces internal ablation. Furthermore, the roof of the conduit could collapse, leading to the formation of ice cliffs and new ponds, which would accelerate the ablation of the debris-covered glacier.