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- Model:SimClast + ( *Fluvial/alluvial processes; **Aggrading … </br>*Fluvial/alluvial processes;</br>**Aggrading fluvial channels in one gridcell with crevasse. Subgrid sedimentation mimics alluvial ridge aggradation and overbank deposition. Avulsions are modelled one dimensionally by calculating the flow and sediment transport at prospective avulsion nodes. See also Dalman & Weltje (2008).</br>*Floodplain processes;</br>**Differential compaction, groundwater table, peat growth and overbank deposition</br>*Hypopycnal plume and marine currents:</br>**Rivers deliver sediment and water to the sea, where the river momentum spreads the suspended sediment in a plume. Multiple plumes and longshore current hydrodynamics are calculated using a potential flow routine. Subsequent sedimentation due to fallout uses the removal rate principle after Syvitski et al (1988).</br>*Wave resuspension and crosshore transport;</br>**Waves are modelled using linear Airy and Stokes wave theory. Deepwater wave height is derived from a Gaussian distribution to represent natural storm variability The asymmetric waves preferentially transport the sands (bedload fraction) shorewards and the fines (suspended load fraction) offshore. In combination with a littoral drift routine this allows waves to rework and transport sediments.</br>allows waves to rework and transport sediments. )
