Modeling of a mixed?load fluvio?deltaic system

Present?day observations and classical classification schemes of alluvial deltas address feeder channel dynamics and multiple sediment fractions. However, high?resolution physics?based mathematical models have not been applied to address formation of both fluvio?deltaic links (channels) and nodes (diffluences and confluences), and their...

Climate change impact on the deltas of Ebro, Po and Rhone: Conceptual models for coastal fringes’ response

All the Mediterranean Dehas are submitted to a physical regression of their coastal fringes and dominated by the wave action because of the decreased water and sediment discharges, if compared to previous stages of their histories. The decrease of the discharges is a consequence of water and solid retention and deviation in the continental...