Hydrologic signatures are metrics that quantify aspects of streamflow response. Linking
signatures to underlying processes enables multiple applications, such as selecting …

The bedrock controls on catchment mixing, storage, and release have been actively studied
in recent years. However, it has been difficult to find neighbouring catchments with …

Surface topography is an important source of information about the functioning and form of a
hydrological landscape. Because of its key role in explaining hydrological processes and …

The substantial tree-to-tree variability of transpiration poses a major challenge to a reliable
stand-scale quantification of transpiration. The diameter at breast height (DBH) and …

The phrase form and function was established in architecture and biology and refers to the
idea that form and functionality are closely correlated, influence each other, and co-evolve …

The role of landscape topography in mediating subsurface water availability and ultimately
tree transpiration is still poorly understood. To assess how hillslope position affects tree …

Hillslopes exert critical controls on the quality and quantity of downstream waters. To
understand and model dominant headwater catchment processes, we need to estimate the …

This research introduces a novel nonlinear Muskingum model for river flood routing, aiming
to enhance accuracy in modeling. It integrates lateral inflows using the Whale Optimization …

Spatial and temporal distributions of soil moisture are important for explaining hydrological
processes at the hillslope scale. The fate of various hillslope flow paths can vary seasonally …

Catchment travel time distributions (TTDs) are an efficient concept for summarizing the time-
varying 3D transport of water and solutes towards an outlet in a single function of a water …