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In mountain, snow driven catchments, snowmelt is supposed to be the primary contribution to river streamflows during spring. In these catchment the contribution of groundwater is not well documented because of the difficulty to monitor groundwater in such complex environment with deep aquifers. In this study we use an integrated hydrologic model to conduct numerical experiments that help quantify the effect of lateral groundwater flow on total annual and peak streamflow in pre-development conditions. Our simulations focus on the Upper C
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