Hydroclimatic changes associated with global warming over the past 50 years have been
documented widely, but physical landscape responses are poorly understood thus far …

Channel networks are key to coastal wetland functioning and resilience under climate
change. Vegetation affects sediment and hydrodynamics in many different ways, which calls …

Our current understanding of semiarid ecosystems is that they tend to display higher
vegetation greenness on polar‐facing slopes (PFS) than on equatorial‐facing slopes (EFS) …

Soil‐mantled pole‐facing hillslopes on Earth tend to be steeper, wetter, and have more
vegetation cover compared with adjacent equator‐facing hillslopes. These and other slope …

Hillslopes constitute the majority of Earth's land surface area and dominate the supply of
sediment to rivers. Hillslope sediment transport is commonly modeled with a rate law that …

In steep landscapes, wildfire‐induced changes to soil and vegetation can lead to extreme
and hazardous geomorphic responses, including debris flows. The wildfire‐induced …

The structure of the critical zone (CZ) is a product of feedbacks among hydrologic, climatic,
biotic, and chemical processes. Past research within snow‐dominated systems has shown …

Solar radiation has a clear signature on the spatial organization of ecohydrologic fluxes,
vegetation patterns and dynamics, and landscape morphology in semiarid ecosystems …

The temporal dynamics of stream networks are vitally important for understanding hydrologic
processes including surface water and groundwater interaction and hydrograph recession …

Composite volcanoes are dynamic landforms that require comprehensive morphological
analysis to understand their formation, degradation and associated controlling processes …