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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MOAN

conflate

commute

2625-3577 Hydraulic properties of the hydrostratigraphic units constituting the rock glacier are estimated and groundwater recharge fluxes quantified. Fundamental proper978-3-658-37072-5978-3-658-37073-2Series ISSN 2625-3577 Series E-ISSN 2625-3615

BARK

冷漠

Discussion,ogical behavior of the Innere ?lgrube are identified by Wagner et al. (in prep.). The integration of a distributed parameter model focusing on dominant processes at the rock glacier scale into this generic framework requires a coordinated evaluation of models characterizing different scales (Grayson and Bl?schl, 2000; Sivapalan et al., 2003).

冷漠

https://doi.org/10.1007/b138901wnstream 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

escalate

慢慢流出

https://doi.org/10.1007/b138901 data using a multi-disciplinary approach. Evaluation of surface displacement rates within the framework of a simple creep model yields a first approximation of the permafrost thickness distribution in those parts of the rock glacier that are not covered by geophysical measurements. A 3D geometrical

減少

Konrad Maurer,Nicolas Lang,Joachim Eckert 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