Simulating glacier mass balance in the cross-border Poiqu/Bhotekoshi Basin, China and Nepal

To assess the change of glacier mass balance (GMB) in the Poiqu/Bhotekoshi basin in the context of global warming, this study applied a conceptual Hydrologiska Bryans Vattenbalansavdelning (HBV) hydrological model to quantify the GMB in the area. The HBV model was trained and validated based on in-s...

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Autores principales: Bo Kong, Huan Yu, Wei Deng, Qing Wang
Formato: article
Lenguaje:EN
Publicado: IWA Publishing 2021
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Acceso en línea:https://doaj.org/article/a4dc644c5e4149f1a52226580f16fc5e
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spelling oai:doaj.org-article:a4dc644c5e4149f1a52226580f16fc5e2021-11-05T19:01:29ZSimulating glacier mass balance in the cross-border Poiqu/Bhotekoshi Basin, China and Nepal2040-22442408-935410.2166/wcc.2020.024https://doaj.org/article/a4dc644c5e4149f1a52226580f16fc5e2021-08-01T00:00:00Zhttp://jwcc.iwaponline.com/content/12/5/1515https://doaj.org/toc/2040-2244https://doaj.org/toc/2408-9354To assess the change of glacier mass balance (GMB) in the Poiqu/Bhotekoshi basin in the context of global warming, this study applied a conceptual Hydrologiska Bryans Vattenbalansavdelning (HBV) hydrological model to quantify the GMB in the area. The HBV model was trained and validated based on in-situ hydro meteorological data from 10 weather stations in the basin. The dataset, which consists of the daily observations for both rainfall and air temperature, was partitioned into two decades, 1988–1998 and 1999–2008 for calibration and validation, respectively. The calibrated model was adopted to restore the daily runoff depth and then estimate the annual changes of GMB in Poiqu/Bhotekoshi basin over the period of 1988–2008. Results show that the Nash–Sutcliffe efficiency coefficient (Reff) of the daily runoff depth simulation after the runoff calibration process was above 0.802. Therefore, the simulated values of the HBV model are reliable and can be used to estimate the GMB of Himalayan cross-border glacial mountain basins with huge elevation difference, and provide scientific data support for water resources management. Furthermore, the result demonstrated a slow year-by-year rise of snow water equivalent because of global warming, and it highly correlates with the soil moisture, the spring temperature and the summer precipitation. HIGHLIGHTS The HBV model had a better simulation effect on the annual daily runoff depth.; The HBV model parameter combination was obtained through calibration.; The precipitation increase was found to have a contribution rate of 38% to runoff.; Glacial melting caused by temperature had a contribution rate of 62% to runoff increase.;Bo KongHuan YuWei DengQing WangIWA Publishingarticleconceptual hydrological modelcross-border riversglacier mass balancepoiqu/bhotekoshi basinrunoff depthEnvironmental technology. Sanitary engineeringTD1-1066Environmental sciencesGE1-350ENJournal of Water and Climate Change, Vol 12, Iss 5, Pp 1515-1531 (2021)
institution DOAJ
collection DOAJ
language EN
topic conceptual hydrological model
cross-border rivers
glacier mass balance
poiqu/bhotekoshi basin
runoff depth
Environmental technology. Sanitary engineering
TD1-1066
Environmental sciences
GE1-350
spellingShingle conceptual hydrological model
cross-border rivers
glacier mass balance
poiqu/bhotekoshi basin
runoff depth
Environmental technology. Sanitary engineering
TD1-1066
Environmental sciences
GE1-350
Bo Kong
Huan Yu
Wei Deng
Qing Wang
Simulating glacier mass balance in the cross-border Poiqu/Bhotekoshi Basin, China and Nepal
description To assess the change of glacier mass balance (GMB) in the Poiqu/Bhotekoshi basin in the context of global warming, this study applied a conceptual Hydrologiska Bryans Vattenbalansavdelning (HBV) hydrological model to quantify the GMB in the area. The HBV model was trained and validated based on in-situ hydro meteorological data from 10 weather stations in the basin. The dataset, which consists of the daily observations for both rainfall and air temperature, was partitioned into two decades, 1988–1998 and 1999–2008 for calibration and validation, respectively. The calibrated model was adopted to restore the daily runoff depth and then estimate the annual changes of GMB in Poiqu/Bhotekoshi basin over the period of 1988–2008. Results show that the Nash–Sutcliffe efficiency coefficient (Reff) of the daily runoff depth simulation after the runoff calibration process was above 0.802. Therefore, the simulated values of the HBV model are reliable and can be used to estimate the GMB of Himalayan cross-border glacial mountain basins with huge elevation difference, and provide scientific data support for water resources management. Furthermore, the result demonstrated a slow year-by-year rise of snow water equivalent because of global warming, and it highly correlates with the soil moisture, the spring temperature and the summer precipitation. HIGHLIGHTS The HBV model had a better simulation effect on the annual daily runoff depth.; The HBV model parameter combination was obtained through calibration.; The precipitation increase was found to have a contribution rate of 38% to runoff.; Glacial melting caused by temperature had a contribution rate of 62% to runoff increase.;
format article
author Bo Kong
Huan Yu
Wei Deng
Qing Wang
author_facet Bo Kong
Huan Yu
Wei Deng
Qing Wang
author_sort Bo Kong
title Simulating glacier mass balance in the cross-border Poiqu/Bhotekoshi Basin, China and Nepal
title_short Simulating glacier mass balance in the cross-border Poiqu/Bhotekoshi Basin, China and Nepal
title_full Simulating glacier mass balance in the cross-border Poiqu/Bhotekoshi Basin, China and Nepal
title_fullStr Simulating glacier mass balance in the cross-border Poiqu/Bhotekoshi Basin, China and Nepal
title_full_unstemmed Simulating glacier mass balance in the cross-border Poiqu/Bhotekoshi Basin, China and Nepal
title_sort simulating glacier mass balance in the cross-border poiqu/bhotekoshi basin, china and nepal
publisher IWA Publishing
publishDate 2021
url https://doaj.org/article/a4dc644c5e4149f1a52226580f16fc5e
work_keys_str_mv AT bokong simulatingglaciermassbalanceinthecrossborderpoiqubhotekoshibasinchinaandnepal
AT huanyu simulatingglaciermassbalanceinthecrossborderpoiqubhotekoshibasinchinaandnepal
AT weideng simulatingglaciermassbalanceinthecrossborderpoiqubhotekoshibasinchinaandnepal
AT qingwang simulatingglaciermassbalanceinthecrossborderpoiqubhotekoshibasinchinaandnepal
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