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From CSDMS
No but possible +
No but possible +
No but possible +
Single Processor +
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23:30:13, 19 February 2009 +
AMASSED; STRATAFORM; EUROSTRATAFORM +
AMASSED; STRATAFORM; EUROSTRATAFORM +
Measured or artificially generated wave and current forcing. Floc diameter, density. Downslope gravity. Vertical grid mesh. Erodibility. Parameters for Bingham rheology. +
mixture equations (derived from two-phase theory with fine sediment assumption). k-epsilon closure derived from two-phase theory. Bingham rheology. Floc property is based on fractal structure. Bottom boundary condition for mud is based on type I erosion. +
Wave-current BL, lengthscale ~1 m nearbed, grid size ~1mm; Tidal BL: lengthscale 10 m, grid size 1cm +
Major quantities: mud floc concentration, flow velocity in longshelf and cross-shelf direction. Other quantities: TKE, turbulent dissipation rate, floc size (if floc dynamics turn on), bottom stress. +
Typical Matlab or Excell plotting +
wave-current boundary layer and fluid mud transport. dilute suspension. wave-supported gravity-driven mudflow. turbulence modulation due to sediment. tidal-driven fluid mud transport. Floc dynamics. Rheology. +
Wave-current BL: timescale ~10 min; time step ~0.01 sec; Tidal BL: timescale days and time step 10 s +
This is a 1DV wave-phase resolving numeric … This is a 1DV wave-phase resolving numerical model for fluid mud transport based on mixture theory with boundary layer approximation. The model incorporates turbulence-sediment interaction, gravity-driven flow, mud rheology, bed erodibility and the dynamics of floc break-up and aggregation.dynamics of floc break-up and aggregation. +
Tian-Jian +
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ASCII +
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0 +
~2Mb +
Coastal +
As code +
fluid mud transport +
Single +
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02:14:24, 17 September 2020 +
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Wave-phase resolving numerical model for fluid mud transport +
ASCII +
365 Weil Hall +
FL +
false +
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Other +
Fortran77 +
Few hours +
2005 +
Model developer +
Matlab +
