A river long profile and its associated channel gradient (measured pixel-to-pixel). Note the
noise in the gradient data, and the increasing gradient as one moves towards the headwaters. …

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

Amplified warming of high latitudes and rapid thaw of frozen ground threaten permafrost
carbon stocks. The presence of permafrost modulates water infiltration and flow, as well as …

The bulk of the crustal shortening across the Himalayas is accommodated across the Main
Frontal Thrust (MFT), forming the topographic ridges of the Siwalik Hills. Here, we quantify …

Quantitative descriptions of stream network and river catchment characteristics provide
valuable context for enabling geomorphologically-informed sustainable river management. For …

River profile analysis has been used extensively in the earth sciences. Commonly, exploration
of river profiles requires downloading and processing Digital Elevation Models (DEMs) for …

Computing hydrological fluxes at the Earth's surface is crucial for landscape evolution models,
topographic analysis, and geographic information systems. However, existing formalisms, …