Current and future role of meltwater-groundwater dynamics in a proglacial Alpine outwash plain

Abstract

Abstract. Glaciated alpine catchments are rapidly evolving due to glacier retreat and consequent geomorphological and ecological changes. As more terrain becomes ice free, the interactions between surface and subsurface waters become gradually more significant, leading to potential changes in water storage and release, which in turn may impact ecological, geomorphological and hydrological processes. In this study, we aim to understand the hydrological functioning of outwash plains as glaciers retreat. These constitute a fluvial aquifer which appears as a focal point for water storage and alpine ecology and their dynamics have only rarely been studied. Based on geophysical investigations as well as year-round stream and groundwater observations, we developed a simplified physically-based 3D MODFLOW model and performed an optimized automatic calibration using PEST HP. By comparing the model results to field observations, we highlight the strong interactions between the upstream river and the aquifer, with stream infiltration being the dominant process of recharge. Groundwater exfiltration occurs in the lower half part of the outwash plain, balancing out the amount of river infiltration at a daily time scale. We show that hillslope contributions from rain and snow-melt have little impact on groundwater levels. We also show that outwash plain aquifers can maintain groundwater levels close to the surface even during long dry periods. From a hydrological perspective, we finally explore how new outwash plains may form in the future due to glacier recession and discuss what cascading impact the presence of multiple outwash plains may have in such catchments. We estimate the total dynamic storage of future outwash plains to be about 20 mm and we demonstrate their limited capacity to produce more stream water than what they infiltrate upstream, except for very low river flows (< 150 to 200 L s−1). Below this limit, they can provide limited baseflow on timescales of weeks, thus maintaining some moisture conditions potentially beneficial for proglacial ecosystems. Their role in attenuating floods also appears limited, as less than 0.5 m3 s−1 of river water can be infiltrated. Outwash plains appear therefore to play an important role for alpine ecosystems but have marginal hydrological effects on downstream river discharge.

Physical and chemical characterization of remote coastal aquifers and submarine groundwater discharge from a glacierized watershed

“…Additional advantages of this method are that it provides a representative combined description of aquifer properties over a large spatial scale from a single point measurement and helps resolve issues over the spatial variabilities in aquifer systems that may not be determined by the other methods. Previous work in geologic analogues assigned specific yields on the higher end of our range, typically from 0.15 to 0.25 for sands and gravels (Chen et al, 2010;Mackay et al, 2020;Müller et al, 2023;Nilsson et al, 2007). Further, this technique may also be applied to estimate K near the Wosnesenski River based on the diurnal flood-wave response observed in proximal piezometers during the melt season or after significant rain events.…”

A call for an accurate presentation of glaciers as water resources

“…This is because the flow along the course of a river is also influenced by output fluxes of natural and anthropogenic origins. In particular, river discharge from high alpine catchment contributes to groundwater recharge by stream infiltration (Müller et al, 2023) and is subject to withdrawals for irrigation or seasonal storage in reservoirs (Wortmann et al, 2019). As a result, contribution from glaciers can be overestimated by default with increasing distance from the glaciers (Kaser et al, 2010).…”