Titlebook: Characterizing Groundwater Flow Dynamics and Storage Capacity in an Active Rock Glacier; Simon Seelig Book 2022 The Editor(s) (if applicab

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fleeting

Introduction,wnstream rivers and aquifers. The Alpine climate has been subject to significant changes during the last decades and is expected to be affected by the global climate response to increasing greenhouse gas concentrations during the 21. century (Gobiet et al., 2014). River peak runoff is predicted to s

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Results and Interpretation, points derived from the geophysical profiles, and 5510 surface displacement vectors distributed across the rock glacier surface. Long-term creep rates are calculated using . = 3, . = 2.4·10. Pa.?s., . = 1604 kg?m., and . = 1826.67 kg?m.. The obtained model consists of a set of four continuous surfa

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Melodrama

Outlook, basis for a prospective distributed parameter model complementing the lumped-parameter rainfall-runoff model provided by Wagner et al. (in prep.). The specified aquifer geometry and boundary conditions can be easily integrated into a numerical groundwater flow model. The estimated hydraulic propert

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watertight,

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