regimeflow
Regimeflow is a term used in hydrology and geomorphology to describe changes in the dominant processes that shape a river's channel or a landscape over time. It refers to a shift from one set of geomorphic conditions and processes to another, often driven by changes in external factors. These external factors can include alterations in water flow, sediment supply, land use, or climate.
When a river experiences a regimeflow, the fundamental ways in which it erodes, transports, and deposits sediment
Understanding regimeflow is crucial for predicting how landscapes will evolve and for managing water resources and