In recent years, the wealth of technological development revolutionised our ability to collect
data in geosciences. Due to the unprecedented level of detail of these datasets …

Landscape morphology reflects the spatial and temporal history of erosion. Erosion in turn
embodies the competition between tectonic and climatic processes. Quantitative analysis of …

Hilltop curvature (CHT) can record erosional responses to tectonic forces and/or climate
change. Although CHT has a linear relationship with the erosion rate, which is a significant …

The Arctic is experiencing rapid climate change, and the effect on hydrologic processes and
resulting geomorphic changes to hillslopes and channels is unclear because we lack …

The generation of Digital Elevation Models (DEMs) through stereogrammetry of optical
satellite images has gained great popularity across various disciplines. For the analysis of …

Resolving Earth's surface at the meter scale is essential for an improved understanding of
the dynamics of mass‐movement processes. In this study, we explore the applicability and …

Episodic landslides supply vast quantities of debris from hillslopes to channels, resulting in
the dilution of cosmogenic nuclides in fluvial sediment. This study revisited the nuclide …

Area‐slope scaling is an important tool for analysing geomorphic processes. In this study,
we used hierarchical clustering to sort the area‐slope scaling data for both the numerical …

Landscape evolution models (LEMs) are prime tools for simulating the evolution of source-to-
sink systems through ranges of spatial and temporal scales. A plethora of various empirical …

Large earthquakes can contribute to mountain growth by building topography but also
contribute to mass removal from mountain ranges through widespread mass wasting. On …