Evolution of river bed morphology is characterized by "erosion in flood season and deposition in dry season".
The complex multi-directional interactions between hydrological, biological and fluvial processes govern the formation and evolution of river landscapes.
Here, we present a geomorphological analysis of the Ethiopian Highlands supplying new constraints on the evolution of river network.
A numerical study was undertaken to investigate non linearity and the potential for self-organized criticality (SOC) in the evolution of river basins.
This study quantified the evolution of river channel and floodplain geometry during a repeated series of hypothetical extreme floods using a 2D full hydro-morphodynamic model (LHMM).
Macrophyte responses to disturbance provide a short-term opportunity to document and interpret plant succession and related hydrogeomorphological interactions relative to the long-term, concomitant evolution of river morphology.
The approach was applied to the long-term hydrological time series to investigate the evolution of river-floodplain relation in Dongting Lake in the last five decades, during which the Yangtze River system experienced unprecedented anthropogenic manipulations.
Despite partially ambiguous results, our analysis nonetheless provides insight into the evolution of river dolphins.
This mostly allopatric distribution pattern indicates that speciation in Iberian barbels follows the evolution of river basins [ 23, 24, 26– 28].
Study on calcite precipitation has major implications for both the hydrochemical evolutions of river systems and the global carbon cycle.
Abad and Garcia [2004, Conceptual and mathematical model for evolution of meandering rivers in naturalization processes.
