Abstract
Climate change is a major concern for freshwater allocation and management, but there is a lack of attention regarding how water impoundment impacts boreal climate at the intersection of mountain topography. We explore how the local climate was affected by the construction of one of North America’s largest reservoirs, the Williston Hydropower Reservoir, in British Columbia’s Rocky Mountain Trench. High-resolution simulations of the Weather Research and Forecasting model over a 10-year period were used to analyze differences in mean meteorological states with and without the reservoir represented in the landscape. Relative to terrain without the Williston Reservoir, autumn precipitation increased by up to 30 mm (11.5%); however, a substantial precipitation decrease in summer results in a 15% reduction of mean annual precipitation over ridges east of the reservoir. The presence of the reservoir with high thermal inertia in place of vegetated soil reduced convection in the warm season so that heavy precipitation events (> 20 mm) become fewer. An increase in mean annual air temperature within 10 km of the reservoir by 0.2–0.5 °C due mainly to significant warming in autumn was also detected. Overland wind increased by 0.5 m s−1 up to 13 km from the reservoir. We highlight the social importance of these results on the perception of environmental change.
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Observational data from weather stations in this study are accessible at https://data.pacificclimate.org/portal/pcds/map/. The datasets generated from WRF and analyzed during the current study are available on demand.
References
Abatzoglou J, Dobrowski S, Parks S et al (2018) TerraClimate, a high-resolution global dataset of monthly climate and climatic water balance from 1958–2015. Sci Data 5:170191. https://doi.org/10.1038/sdata.2017.191
Aravind A, Srinivas CV, Shrivastava R et al (2022) Simulation of atmospheric flow field over the complex terrain of Kaiga using WRF: sensitivity to model resolution and PBL physics. Meteorol Atmos Phys 134:13. https://doi.org/10.1007/s00703-021-00848-4
Bigler C, Gavin DG, Gunning C, Veblen TT (2007) Drought induces lagged tree mortality in a subalpine forest in the Rocky Mountains. Oikos 116:1983–1994. https://doi.org/10.1111/j.2007.0030-1299.16034.x
Coop JD, Parks SA, Stevens-Rumann CS et al (2020) Wildfire-driven forest conversion in western North American landscapes. BioScience 70(8):659–673. https://doi.org/10.1093/biosci/biaa061
Crampton C (1992) Problems of environmental conservation for the Sekani Ingenika Band in Northern British Columbia, Canada. Environ Conserv 19:76–77. https://doi.org/10.1017/S0376892900030290
Degu AM, Hossain F, Niyogi D et al (2011) The influence of large dams on surrounding climate and precipitation patterns. Geophys Res Lett 38:L04405. https://doi.org/10.1029/2010GL046482
Ebrahimi S, Marshall SJ (2016) Surface energy balance sensitivity to meteorological variability on Haig Glacier, Canadian Rocky Mountains. Cryosphere 10:2799–2819. https://doi.org/10.5194/tc-10-2799-2016
Environment and Climate Change Canada (2022) Station results - historical data, Ingenika Point, pp 1973–1983. https://climate.weather.gc.ca/historical_data/search_historic_data_e.html
Gu H, Jin J, Wu Y et al (2015) Calibration and validation of lake surface temperature simulations with the coupled WRF-Lake model. Clim Change 129:471–483. https://doi.org/10.1007/s10584-013-0978-y
Hersbach H, Bell B, Berrisford P et al (2020) The ERA5 global reanalysis. Q J R Meteorol Soc 146(730):1999–2049. https://doi.org/10.1002/qj.3803
Hossain F, Degu AM, Yigzaw W et al (2012) Climate feedback–based provisions for dam design, operations, and water management in the 21st century. J Hydrol Eng 17:837–850. https://web.archive.org/web/20170811094645id_/https://climate.agry.purdue.edu/climate/dev/publications-protected/j123.pdf
Huziy O, Sushama L (2016) Impact of lake–river connectivity and interflow on the Canadian RCM simulated regional climate and hydrology for Northeast Canada. Clim Dynam 48:709–725. https://doi.org/10.1007/s00382-016-3104-9
Iakunin M, Abreu EFM, Canhoto P et al (2022) Impact of a large artificial lake on regional climate: a typical meteorological year Meso-NH simulation results. Int J Climatol 42(2):1231–1252. https://doi.org/10.1002/joc.7299
International Commission on Large Dams (2020) Number of Dams by Country Members. https://www.icold-cigb.org/article/GB/world_register/general_synthesis/number-of-dams-bycountry-members
Irambona C, Music B, Nadeau DF et al (2018) Impacts of boreal hydroelectric reservoirs on seasonal climate and precipitation recycling as simulated by the CRCM5: a case study of the La Grande River watershed, Canada. Theor Appl Climatol 131:1529–1544. https://doi.org/10.1007/s00704-016-2010-8
Keane RE, Mahalovich MF, Bollenbacher BL et al (2018) Effects of climate change on forest vegetation in the northern Rockies. In: Halofsky J, Peterson D (eds) Climate change and Rocky Mountain ecosystems, Advances in global change research. Springer, Cham, pp 59–95. https://doi.org/10.1007/978-3-319-56928-4_5
Kochendorfer J, Earle M, Rasmussen R et al (2022) How well are we measuring snow postSPICE? Bull Am Meteorol Soc 102:1–49. https://doi.org/10.1175/BAMS-D-20-0228
Leung LR, Qian Y (2003) The sensitivity of precipitation and snowpack simulations to model resolution via nesting in regions of complex terrain. J Hydrometeor 4:1025–1043. https://doi.org/10.1175/1525-7541(2003)004<1025:TSOPAS>2.0.CO;2
Lofgren BM (1997) Simulated effects of idealized Laurentian Great Lakes on regional and large-scale climate. J Clim 10:2847–2858. https://doi.org/10.1175/1520-0442(1997)010<2847:SEOILG>2.0.CO;2
Loo T (2007) Disturbing the peace: environmental change and the scales of justice on a northern river. Environ Hist 12:895–919. https://doi.org/10.1093/envhis/12.4.89
Ma ZH, Peng CH, Zhu QA et al (2012) Regional drought-induced reduction in the biomass carbon sink of Canada's boreal forests. Proc Natl Acad Sci USA 109(7):2423–2427. https://doi.org/10.1073/pnas.1111576109
Muñoz-Sabater J (2021) ERA5-Land monthly averaged data from 1950 to present. Copernicus Climate Change Service (C3S) Climate Data Store (CDS). (Accessed on 11-11-2022). https://doi.org/10.24381/cds.68d2bb30
Nordbo A, Launiainen S, Mammarella I et al (2011) Long-term energy flux measurements and energy balance over a small boreal lake using eddy covariance technique. J Geophys Res-Atmos 116:D02119. https://doi.org/10.1029/2010JD014542
Notaro M, Holman K, Zarrin A et al (2013) Influence of the Laurentian Great Lakes on regional climate. J Clim 26(3):789–804. https://doi.org/10.1175/JCLI-D-12-00140.1
Pal S, Lee TR, Phelps S, De Wekker SFJ (2014) Impact of atmospheric boundary layer depth variability and wind reversal on the diurnal variability of aerosol concentration at a valley site. Sci Total Environ 496:424–434. https://doi.org/10.1016/j.scitotenv.2014.07.067
Pouliot D, Latifovic R (2018) Reconstruction of Landsat time series in the presence of irregular and sparse observations: development and assessment in north-eastern Alberta, Canada. Remote Sens Environ 204:979–996. https://doi.org/10.1016/j.rse.2017.07.036
Python Software Foundation (2022) Python Language Reference, version 3.8.8. http://www.python.org
Rudisill W, Flores A, McNamara J (2021) The impact of initial snow conditions on the numerical weather simulation of a northern rockies atmospheric river. J Hydrometeorol 22:155–167. https://doi.org/10.1175/JHM-D-20-0018.1
Schirmer M, Jamieson M (2014) Verification of analysed and forecasted winter precipitation in complex terrain. Cryosphere 9:587–601. https://doi.org/10.5194/tc-9-587-2015
Schoennagel T, Veblen TT, Romme WH et al (2005) Enso and pdo variability affect drought-induced fire occurrence in Rocky Mountain subalpine forests. Ecol Appl 15:2000–2014. https://doi.org/10.1890/04-1579
Skamarock WC, Klemp JB, Dudhia J, et al. (2021) A Description of the Advanced Research WRF Version 4. https://opensky.ucar.edu/islandora/object/opensky:2898
Smith RB (2019) 100 years of progress on mountain meteorology research. Meteorol Monogr 59. https://doi.org/10.1175/AMSMONOGRAPHS-D-18-0022.1
Stockner J, Langston A, Sebastian D, Wilson G (2005) The limnology of Williston Reservoir: British Columbia’s largest lacustrine ecosystem. Water Qual Res J Canada 40:28–50. https://www.cawq.ca/journal/temp/article/177.pdf
Subin ZM, Murphy LN, Li F et al (2012a) Boreal lakes moderate seasonal and diurnal temperature variation and perturb atmospheric circulation: analyses in the Community Earth System Model 1 (CESM1). Tellus A 64(1):15639. https://doi.org/10.3402/tellusa.v64i0.15639
Subin ZM, Riley WJ, Mironov D (2012b) An improved lake model for climate simulations: model structure, evaluation, and sensitivity analyses in CESM1. J Adv Model Earth Syst 4:M02001. https://doi.org/10.1029/2011MS000072
Thiery W, Davin EL, Panitz HJ et al (2015) The impact of the African Great lakes on the regional climate. J Clim 28(10):4061–4085. https://doi.org/10.1175/JCLI-D-14-00565.1
Thornton MM, Shrestha R, Wei Y et al (2020) Daymet: daily surface weather data on a 1-km grid for North America, version 4. ORNL DAAC, Oak Ridge, Tennessee, USA. https://doi.org/10.3334/ORNLDAAC/1840
USGS (2015) Global land cover characteristics data base version 2.0. https://lta.cr.usgs.gov/glcc/globdoc2_0. Accessed 13 Oct 2021
Vanderkelen I, van Lipzig NPM, Sacks WJ et al (2021) Simulating the impact of global reservoir expansion on the present-day climate. J Geophys Res-Atmos 126:e2020JD034485. https://doi.org/10.1029/2020JD034485
Wang F, Ni G, Riley WJ et al (2019) Evaluation of the WRF lake module (v1.0) and its improvements at a deep reservoir. Geosci Model Dev 12:2119–2138. https://doi.org/10.5194/gmd-12-2119-2019
Wang X, Wang W, He Y et al (2023) Numerical simulation of thermal stratification in Lake Qiandaohu using an improved WRF-Lake model. J Hydrol 618:129184. https://doi.org/10.1016/j.jhydrol.2023.129184
Winchester J, Mahmood R, Rodgers W et al (2017) A model-based assessment of potential impacts of man-made reservoirs on precipitation. Earth Interact 21:1–31. https://doi.org/10.1175/EI-D-16-0016.1
Woldemichael AT, Hossain F, Pielke R Sr (2014a) Impacts of postdam land use/land cover changes on modification of extreme precipitation in contrasting hydroclimate and terrain features. J Hydrometeorol 15:777–800. https://doi.org/10.1175/JHM-D-13-085.1
Woldemichael AT, Hossain F, Pielke R Sr (2014b) Evaluation of surface properties and atmospheric disturbances caused by post-dam alterations of land use/land cover. Hydrol Earth Syst Sci 18:3711–3732. https://doi.org/10.5194/hess-18-3711-2014
Woldemichael AT, Hossain F, Pielke R Sr, Beltrán-Przekurat A (2012) Understanding the impact of dam-triggered land use/land cover change on the modification of extreme precipitation. Water Resour Res 48:W09547. https://doi.org/10.1029/2011WR011684
Wu J, Gao X, Giorgi F et al (2012) Climate effects of the Three Gorges Reservoir as simulated by a high resolution double nested regional climate model. Quat Int 282(19):27–26. https://doi.org/10.1016/j.quaint.2012.04.028
Wu Y, Huang A, Lazhu et al (2020) Improvements of the coupled WRF-Lake model over Lake Nam Co, Central Tibetan Plateau. Clim Dyn 55:2703–2724. https://doi.org/10.1007/s00382-020-05402-3
Xiao C, Lofgren BM, Wang J, Chu PY (2016) Improving the lake scheme within a coupled WRF-lake model in the Laurentian Great Lakes. J Adv Model Earth Syst 8:1969–1985. https://doi.org/10.1002/2016MS000717
Yigzaw W, Hossain F (2014) Leveraging precipitation modification around large reservoirs in orographic environments for water resources management. J Civil Environ Eng 4(5). https://pdfs.semanticscholar.org/5a2c/60cf13f7eb4fb9964fac5e00e110dc8055d4.pdf?_ga=2.5704626 0296.32906658.1642744620-848135205.1642744620
Zhang H, Pu Z, Zhang X (2013) Examination of errors in near-surface temperature and wind from WRF numerical simulations in regions of complex terrain. Wea Forecasting 28:893–914. https://doi.org/10.1175/WAF-D-12-00109.1
Zhang X, Alexander L, Hegerl GC et al (2011) Indices for monitoring changes in extremes based on daily temperature and precipitation data. WIREs Climate Change 2(6):851–870. https://doi.org/10.1002/wcc.147
Zhirnova DF, Belokopytova LV, Meko DM et al (2021) Climate change and tree growth in the Khakass-Minusinsk Depression (South Siberia) impacted by large water reservoirs. Sci Rep 11:14266. https://doi.org/10.1038/s41598-021-93745-0
Acknowledgements
We acknowledge the support of high-performance computing resources from the University of Northern British Columbia.
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This study was supported by funding from Mitacs, Chu Cho Environmental, and Crown-Indigenous Relations and Northern Affairs Canada, as well as through NSERC Discovery Grants to P. Jackson and B. Menounos.
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All authors contributed to the study’s conception and design. Material preparation, data collection, and analysis were performed by CO. The first draft of the manuscript was written by CO and all authors commented on and edited previous versions of the manuscript. All authors read and approved the final manuscript.
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Onwukwe, C., Jackson, P.L., Islam, S.u. et al. Climatic effects of the Williston Reservoir on Tsay Keh Dene Nation Territory of northern British Columbia, Canada. Climatic Change 177, 23 (2024). https://doi.org/10.1007/s10584-024-03683-9
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DOI: https://doi.org/10.1007/s10584-024-03683-9