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

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,...
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Autor*in:	A. Parajuli [verfasserIn] M. B. Chand [verfasserIn] R. B. Kayastha [verfasserIn] J. M. Shea [verfasserIn] P. K. Mool [verfasserIn]

Format:	E-Artikel
Sprache:	Englisch

Erschienen:	2015

Übergeordnetes Werk:	In: Proceedings of the International Association of Hydrological Sciences - Copernicus Publications, 2017, 368(2015), Seite 409-414
Übergeordnetes Werk:	volume:368 ; year:2015 ; pages:409-414

Links:	Link aufrufen Link aufrufen Link aufrufen Journal toc Journal toc

DOI / URN:	10.5194/piahs-368-409-2015

Katalog-ID:	DOAJ025504657

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callnumber-first	G - Geography, Anthropology, Recreation
author	A. Parajuli
spellingShingle	A. Parajuli misc GE1-350 misc QE1-996.5 misc Environmental sciences misc Geology Modified temperature index model for estimating the melt water discharge from debris-covered Lirung Glacier, Nepal
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topic_title	GE1-350 QE1-996.5 Modified temperature index model for estimating the melt water discharge from debris-covered Lirung Glacier, Nepal
topic	misc GE1-350 misc QE1-996.5 misc Environmental sciences misc Geology
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title	Modified temperature index model for estimating the melt water discharge from debris-covered Lirung Glacier, Nepal
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title_full	Modified temperature index model for estimating the melt water discharge from debris-covered Lirung Glacier, Nepal
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title_sort	modified temperature index model for estimating the melt water discharge from debris-covered lirung glacier, nepal
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title_auth	Modified temperature index model for estimating the melt water discharge from debris-covered Lirung Glacier, 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 km<sup<2</sup<, and a debris-covered glacier area, 1.13 km<sup<2</sup<. 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 R<sup<2</sup< 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.
abstractGer	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 km<sup<2</sup<, and a debris-covered glacier area, 1.13 km<sup<2</sup<. 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 R<sup<2</sup< 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.
abstract_unstemmed	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 km<sup<2</sup<, and a debris-covered glacier area, 1.13 km<sup<2</sup<. 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 R<sup<2</sup< 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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title_short	Modified temperature index model for estimating the melt water discharge from debris-covered Lirung Glacier, Nepal
url	https://doi.org/10.5194/piahs-368-409-2015 https://doaj.org/article/f49c76ecca314afab9f0cb0b9ebe9501 https://www.proc-iahs.net/368/409/2015/piahs-368-409-2015.pdf https://doaj.org/toc/2199-8981 https://doaj.org/toc/2199-899X
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Modified temperature index model for estimating the melt water discharge from debris-covered Lirung Glacier, Nepal

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