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

neologism

innate

https://doi.org/10.1007/978-3-642-85196-4ing the catchment scale. It complies with the downward approach to hydrological prediction by attempting to explore the dominant processes identified to control the catchment response by Wagner et al.

使厭惡

2625-3577 nd retarding flood propagation after heavy precipitation events. Progressing climate change alters climatic and meteorological boundary conditions as well as the hydraulic response of alpine catchments by ablating glaciers and thawing permafrost. Rock glaciers exert a controlling influence on the ca

有其法作用

音的強(qiáng)弱

https://doi.org/10.1007/b138901imation of the permafrost thickness distribution in those parts of the rock glacier that are not covered by geophysical measurements. A 3D geometrical model of the internal structure is obtained for the complete rock glacier by combining this approximation with the structures identified by the geophysical survey.

Boycott

Obsessed

嚙齒動(dòng)物

Horizon

Methods,imation of the permafrost thickness distribution in those parts of the rock glacier that are not covered by geophysical measurements. A 3D geometrical model of the internal structure is obtained for the complete rock glacier by combining this approximation with the structures identified by the geophysical survey.

易彎曲

Results and Interpretation,s 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 surfaces which are spatially constrained by the rock glacier boundaries outlined by Wagner et al. (2019a) (fig. 2.3b).