Field measurements were used to quantify suspended sediment yields for 14 sub-catchments within a total catchment area of nearly 1400 km2, including nine catchments defining a nested basin system starting from 1 km2.
The tool is based on the United States Geological Survey (USGS) SPAtially Referenced Regression on Watershed attributes (SPARROW) model and implements the prediction portion of SPARROW to quantify overland and in-stream losses of nitrogen within a river basin system.
It is a Cenozoic foreland basin system.
The Yangtze Fold Zone and the Sichuan Basin represent a retro-arc foreland basin system that is >800 km away from the continental-margin magmatic arc.
Late Quaternary landscape evolution was analysed with reference to a small (0.08 km2) drainage basin system in southeastern Gansu Province, southwestern Chinese Loess Plateau.
The Carpathians Pannonian Basin system provides a natural laboratory for analysing lithospheric to surface controls on tectonic topography development in a coupled source-to-sink environment.
Being Lagrangian in construction, this new model is computationally efficient making it an ideal tool for long term simulation for water resource planning, management and operation decision making in a large and complex river basin system.
The Cretaceous-Tertiary northwest-trending Sirt Basin system, Libya, is a rift/sag basin formed on Pan-African to Paleozoic-aged basement of North Africa.
The Pra Basin is part of the south-western basin system in Ghana and has a drainage area of 23,188 km2 and an estimated mean annual discharge of 214 m3 s−1 (Dickson and Benneh 1980).
