We present a multi-method geophysical approach combining drone-based GPR, ERT with IP, and sMNR to improve subsurface hydrological mapping in a rapidly changing mountain environment.
The cultural loss and damage of glacier retreat demands further attention: A case study from Cerro El Plomo glaciers in Santiago, Chile
We use the case of the retreating glaciers of Cerro El Plomo near Santiago, Chile to call for more collaborative studies between glaciologists, social scientists, and local communities.
Assessing the Added Value of Convection-Permitting Climate Models for Hydrological Extremes in Western Norway
We evaluate CPRCMs for flood simulations in Western Norway, showing improved precipitation representation but highlighting the need for bias correction to enhance flood prediction in mountainous basin
Flow regime changes resulting from land cover and climate change in a watershed spanning the rain-snow transition zone
Streamflow changes resulting from land cover and climate changes strongly depend on spatial scale, vegetation ages, and specific flow metrics.
The paradox of choice: Evaluating climate change projections for hydrological impact models considering uncertainty and spatiotemporal aspects.
The best projection is neither feasible nor foreseen, but this methodology aims to guide a coherent selection of available products or to identify the need to develop new ones
Exploring Bedload Fluxes in Alpine Rivers: Application of the D-CASCADE Model in the Sulden Catchment
We apply the D-CASCADE model to an Alpine river to reconstruct and predict bedload fluxes and sediment connectivity at the network-scale, critical for hazard mitigation and sustainable management.
A forecasting framework for mountain glacier evolution
A self-consistent, ice-dynamic forecasting framework for glacier evolution is presented that generates a 3D digital representation of any glacier on this planet firmly tied to Earth observations.
Evaluation of multi-sources precipitation datasets in ungauged mountainous regions using glacier-hydrological modeling
We evaluate precipitation datasets in an ungauged Tibetan Plateau watershed using WRF-Hydro/Glacier. It shows large uncertainties and the potential of reanalysis datasets for hydrological applications
Landscape geomorphological sensitivity: The paraglacial response of Alpine basins to rapid warming
The paraglacial response of Alpine basins to rapid warming controls sediment export. DoDs from historical photogrammetry were compared to hydropower records to understand processes supplying sediment.
Evaluation of a New Process-Based Snow Accumulation Model in Needleleaf Forests
New snow interception and canopy snow ablation parameterisations are evaluated for estimating subcanopy snow accumulation