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

The rate of sediment supply from erosional catchment to depositional basin depends
primarily upon climate, relief, catchment slope and lithology. It varies in both time and space …

Sediment generation and transport through terrestrial catchments influence soil distribution,
geochemical cycling of particulate and dissolved loads, and the character of the stratigraphic …

Climate, either directly through its expression as temperature and precipitation or indirectly
through its influence on vegetation is a major control on the type and intensity of the various …

Eolian processes and landforms are sensitive to changes in atmospheric parameters and
surface conditions that affect sediment supply and mobility. The response of eolian …

Humans are primary agents of geomorphic change, and rates of anthropogenic landscape
change likely far exceed the pace of change expected from natural geologic processes …

Earth's climate affects nearly all aspects of landscape evolution, from the breakdown of rock
to the delivery of sediment to the oceans. Yet quantifying climate's influence on landscapes …

Climate, tectonics, and life influence the flux and caliber of sediment transported across
Earth's surface. These environmental conditions can leave behind imprints in the Earth's …

Weathering on mountain slopes converts rock to sediment that erodes into channels and
thus provides streams with tools for incision into bedrock. Both the size and flux of sediment …

Climate strongly affects the production of sediment from mountain catchments as well as its
transport and deposition within adjacent sedimentary basins,,. However, identifying climatic …