Application of the HBV model for the future projections of water levels using dynamically downscaled global climate model data

The Hydrologiska Byråns Vattenbalansavdelning (HBV) model was used to project the future water levels of the Mackenzie River at selected stations. The Weather Research and Forecasting (WRF) model was utilized to dynamically downscale the Global Climate Model data. The calibrated and validated HBV mo...

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Autores principales: Lia Pervin, Thian Yew Gan, Hester Scheepers, Md Saiful Islam
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Publicado: IWA Publishing 2021
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spelling oai:doaj.org-article:d036de2cec0240a5a4fd3049561ade302021-11-05T19:07:28ZApplication of the HBV model for the future projections of water levels using dynamically downscaled global climate model data2040-22442408-935410.2166/wcc.2021.302https://doaj.org/article/d036de2cec0240a5a4fd3049561ade302021-09-01T00:00:00Zhttp://jwcc.iwaponline.com/content/12/6/2364https://doaj.org/toc/2040-2244https://doaj.org/toc/2408-9354The Hydrologiska Byråns Vattenbalansavdelning (HBV) model was used to project the future water levels of the Mackenzie River at selected stations. The Weather Research and Forecasting (WRF) model was utilized to dynamically downscale the Global Climate Model data. The calibrated and validated HBV model was run with the WRF downscaled CanESM2 data and with the PCIC data for the historical (1979–2005) period, and then compared with the observed flow data at the Fort Simpson station and the Arctic Red River station. The simulated streamflow showed a good correlation with the observed streamflow (R2 value was around 0.85). The HBV model was then forced with the bias-corrected WRF downscaled daily rainfall and temperature data driven by the CanESM2 RCP 4.5 and RCP 8.5 climate scenarios to simulate the future streamflow for the 2041–2070 period. Rating curves were used to convert streamflow to water levels. At the Fort Simpson station, mean flow was projected to decrease by about 5% under both RCP 4.5 and RCP 8.5 scenarios, whereas the peak flow was likely to reduce by about 12 and 9% for RCP 4.5 and RCP 8.5 scenarios, respectively, in the 2050s. The projected lower water levels could affect the navigability and the northern ferry operations of the Mackenzie River. HIGHLIGHTS In this study, the Global Climate Model data for 2041–2070 were dynamically downscaled into a regional scale by the Weather Research and Forecasting model.; A conceptual hydrological model (HBV) was utilized to simulate the streamflow for the 2050s.; Reduced water levels were projected during the summer season in the 2050s which could affect the northern water transport system of Canada.;Lia PervinThian Yew GanHester ScheepersMd Saiful IslamIWA Publishingarticledownscalingfuture projectiongcmhbv modelwater levelwrf modelEnvironmental technology. Sanitary engineeringTD1-1066Environmental sciencesGE1-350ENJournal of Water and Climate Change, Vol 12, Iss 6, Pp 2364-2377 (2021)
institution DOAJ
collection DOAJ
language EN
topic downscaling
future projection
gcm
hbv model
water level
wrf model
Environmental technology. Sanitary engineering
TD1-1066
Environmental sciences
GE1-350
spellingShingle downscaling
future projection
gcm
hbv model
water level
wrf model
Environmental technology. Sanitary engineering
TD1-1066
Environmental sciences
GE1-350
Lia Pervin
Thian Yew Gan
Hester Scheepers
Md Saiful Islam
Application of the HBV model for the future projections of water levels using dynamically downscaled global climate model data
description The Hydrologiska Byråns Vattenbalansavdelning (HBV) model was used to project the future water levels of the Mackenzie River at selected stations. The Weather Research and Forecasting (WRF) model was utilized to dynamically downscale the Global Climate Model data. The calibrated and validated HBV model was run with the WRF downscaled CanESM2 data and with the PCIC data for the historical (1979–2005) period, and then compared with the observed flow data at the Fort Simpson station and the Arctic Red River station. The simulated streamflow showed a good correlation with the observed streamflow (R2 value was around 0.85). The HBV model was then forced with the bias-corrected WRF downscaled daily rainfall and temperature data driven by the CanESM2 RCP 4.5 and RCP 8.5 climate scenarios to simulate the future streamflow for the 2041–2070 period. Rating curves were used to convert streamflow to water levels. At the Fort Simpson station, mean flow was projected to decrease by about 5% under both RCP 4.5 and RCP 8.5 scenarios, whereas the peak flow was likely to reduce by about 12 and 9% for RCP 4.5 and RCP 8.5 scenarios, respectively, in the 2050s. The projected lower water levels could affect the navigability and the northern ferry operations of the Mackenzie River. HIGHLIGHTS In this study, the Global Climate Model data for 2041–2070 were dynamically downscaled into a regional scale by the Weather Research and Forecasting model.; A conceptual hydrological model (HBV) was utilized to simulate the streamflow for the 2050s.; Reduced water levels were projected during the summer season in the 2050s which could affect the northern water transport system of Canada.;
format article
author Lia Pervin
Thian Yew Gan
Hester Scheepers
Md Saiful Islam
author_facet Lia Pervin
Thian Yew Gan
Hester Scheepers
Md Saiful Islam
author_sort Lia Pervin
title Application of the HBV model for the future projections of water levels using dynamically downscaled global climate model data
title_short Application of the HBV model for the future projections of water levels using dynamically downscaled global climate model data
title_full Application of the HBV model for the future projections of water levels using dynamically downscaled global climate model data
title_fullStr Application of the HBV model for the future projections of water levels using dynamically downscaled global climate model data
title_full_unstemmed Application of the HBV model for the future projections of water levels using dynamically downscaled global climate model data
title_sort application of the hbv model for the future projections of water levels using dynamically downscaled global climate model data
publisher IWA Publishing
publishDate 2021
url https://doaj.org/article/d036de2cec0240a5a4fd3049561ade30
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AT thianyewgan applicationofthehbvmodelforthefutureprojectionsofwaterlevelsusingdynamicallydownscaledglobalclimatemodeldata
AT hesterscheepers applicationofthehbvmodelforthefutureprojectionsofwaterlevelsusingdynamicallydownscaledglobalclimatemodeldata
AT mdsaifulislam applicationofthehbvmodelforthefutureprojectionsofwaterlevelsusingdynamicallydownscaledglobalclimatemodeldata
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