Articles | Volume 25, issue 6
Hydrol. Earth Syst. Sci., 25, 3731–3757, 2021
https://doi.org/10.5194/hess-25-3731-2021
Hydrol. Earth Syst. Sci., 25, 3731–3757, 2021
https://doi.org/10.5194/hess-25-3731-2021

Research article 01 Jul 2021

Research article | 01 Jul 2021

Quantifying floodwater impacts on a lake water budget via volume-dependent transient stable isotope mass balance

Janie Masse-Dufresne et al.

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Cited articles

Ageos: Drinking water supply: Application for an authorization under Section 31 of Groundwater Catchment Regulation: Hydrogeological expert report, 2010-723, volume 1 de 2, AGEOS, Brossard, QC, Canada, 2010. 
Ageos: Drinking water supply: Monitoring of piezometric fluctuations in the water table and lake levels: Period from April 27, 2012 to December 17, 2015: Annual Report 2015, AGEOS, Brossard, QC, Canada, 42 pp., 2016. 
Aissia, M. A. B., Chebana, F., Ouarda, T. B. M. J., Roy, L., Desrochers, G., Chartier, I., and Robichaud, É.: Multivariate analysis of flood characteristics in a climate change context of the watershed of the Baskatong reservoir, Province of Québec, Canada, Hydrol. Process., 26, 130–142, https://doi.org/10.1002/hyp.8117, 2012. 
Arnoux, M., Barbecot, F., Gibert-Brunet, E., Gibson, J., and Noret, A.: Impacts of changes in groundwater recharge on the isotopic composition and geochemistry of seasonally ice-covered lakes: insights for sustainable management, Hydrol. Earth Syst. Sci., 21, 5875–5889, https://doi.org/10.5194/hess-21-5875-2017, 2017a. 
Arnoux, M., Barbecot, F., Gibert-Brunet, E., Gibson, J., Rosa, E., Noret, A., and Monvoisin, G.: Geochemical and isotopic mass balances of kettle lakes in southern Quebec (Canada) as tools to document variations in groundwater quantity and quality, Environ. Earth Sci., 76, 106, https://doi.org/10.1007/s12665-017-6410-6, 2017b. 
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A volume-dependent transient isotopic mass balance model was developed for an artificial lake in Canada, in a context where direct measurements of surface water fluxes are difficult. It revealed that floodwater inputs affected the dynamics of the lake in spring but also significantly influenced the long-term water balance due to temporary subsurface storage of floodwater. Such models are paramount for understanding the vulnerability of lakes to changes in groundwater quantity and quality.