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/s). The predicted increase in hydraulic heads in winter may reach 15 m and the maximum decrease in summer may reach 3 m. Simulations show that winter processes play a key role in the seasonal modifications anticipated for surface and subsurface flow dynamics.
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Cochand et al. (Tue,) studied this question.
www.synapsesocial.com/papers/6a00f8bbef8139f8ff77b4c6 — DOI: https://doi.org/10.1111/gwat.12848
Fabien Cochand
René Therrien
Jean‐Michel Lemieux
Ground Water
Université Laval
University of Neuchâtel
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