Articles | Volume 368
Proc. IAHS, 368, 409–414, 2015
https://doi.org/10.5194/piahs-368-409-2015
Proc. IAHS, 368, 409–414, 2015
https://doi.org/10.5194/piahs-368-409-2015

  07 May 2015

07 May 2015

Modified temperature index model for estimating the melt water discharge from debris-covered Lirung Glacier, Nepal

A. Parajuli1, M. B. Chand1, R. B. Kayastha1, J. M. Shea1, and P. K. Mool2 A. Parajuli et al.
  • 1Himalayan Cryosphere, Climate and Disaster Research Center, Kathmandu University, Dhulikhel, Nepal
  • 2International Centre for Integrated Mountain Development, Lalitpur, Nepal

Abstract. In the Nepalese Himalayas, the complex topography, occurrence of debris covered glaciers, and limited data availability creates substantial difficulties for modelling glacier melt. The proper recognition of melt processes governs the accurate estimation of melt water from glacier dominated systems, even in the presence of debris-covered glaciers. This paper presents a glacier melt model developed for the Lirung sub-basin of Langtang valley, which has both a clean glacier area, 5.86 km2, and a debris-covered glacier area, 1.13 km2. We use a temperature index approach to estimate sub-daily melt water discharge for a two week period at the end of monsoon, and the melt factor is varied according to the aspect and distributed to each grid processed from the digital elevation model. The model uses easily available data and simple extrapolation techniques capable of generating melt with limited data. The result obtained from this method provides accurate estimate with an R2 value of 0.89, bias of 0.9% and Nash-Sutcliffe efficiency of 0.86, and suitable in Himalaya where data availability is major issue.

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