In large sedimentary basins surrounded by mountainous glaciers, mountainous runoff feeding the basin increases as a consequence of enhanced glacier melting. In this context, it woud be useful to assessing this effect if groundwater regime is monitored in regions that are affected, in particular, the alluvial fans.

This qestion intends to stimulate a discussion on this by collecting examples and datasets from different regions to achieve a common understading of the issue.

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