Abstract Models test our understanding of processes and can reach beyond the spatial and
temporal scales of measurements. Multi-component Reactive Transport Models (RTMs) …

The Earth's surface morphology, in an abiotic context, is a consequence of major forcings
such as tectonic uplift, erosion, sediment transport, and climate. Recently, however, it has …

Sediment transport (bedload and suspension) plays a relevant role in the morphological
response of river channels to large floods. Sediment load controls erosion and aggradation …

This revised and updated edition continues to provide a comprehensive introduction to the
subject, exploring the world's landforms from a broad systems perspective. It covers the …

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 …

Gully erosion is a significant environmental concern globally. It reduces agricultural
productivity, damages urban and rural infrastructure, degrades the quality of receiving …

Understanding Earth surface responses in terms of sediment dynamics to climatic variability
and tectonics forcing is hindered by limited ability of current models to simulate long-term …

There is a paradox in the relationship between bedload transport rates and flow variables:
laboratory and field studies have reported on how bedload transport rates depend on flow …

The Mountain Front Flexure marks a dominant topographic step in the frontal part of the
Zagros Fold–Thrust Belt. It is characterized by numerous active anticlines atop of a …

Soil is central in the terrestrial ecosystem, linking and providing feedback responses to the
other components, ie, water, atmosphere, and vegetation. However, the role of soil in …