MIKE 21 specialises in two-dimensional (2D) modelling, offering precise simulations of water flow and movement in coastal areas, estuaries, and rivers. It enables accurate predictions of water levels, currents, temperature variations, and flood occurrences, excelling in managing intricate bathymetry and external forces like wind effects.

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MIKE 21 is a computer program that simulates flows, waves, sediments and ecology in rivers, lakes, estuaries, bays, coastal areas and seas in two dimensions. It was developed by DHI.

The objective of this training example is to set up a simplified MIKE 21 Flow Model for Øresund from scratch and to calibrate the model to a satisfactory level. The exercise has been made as realistic as possible, although some short cuts have been made with respect to the data input.

MIKE 21 SW is a new generation spectral wind-wave model based on unstructured meshes. The model simulates the growth, decay and transformation of wind-generated waves and swell waves in offshore and coastal areas. The directional decoupled parametric formulation is based on a parameterization of the wave action conservation equation.

MIKE 21 is a depth-integrated, two-dimensional flow model. This means that the simulation of the transport of fine-grained material must be averaged over depth and appropriate parameterisations of the sediment processes must be applied.

MIKE 21 SW is a state-of-the-art third generation spectral wind-wave model developed by DHI Water & Environment. The model simulates the growth, decay and transformation of wind-generated waves and swell in offshore and coastal areas.

The following documentation are available for the MIKE 21/3 Integrated Models Products: MIKE 21/3 Coupled Model FM ^ top. MIKE 21/3 Coupled Model FM, User Guide; MIKE 21/3 Coupled Model FM, Step-by-Step Training Guide: Coastal Application; MIKE 21/3 Coupled Model FM, Shoreline Morphology, Step-by-Step Training Guide: Headland Beach example

1992年1月1日 · MIKE 21 is a comprehensive modelling system for the simulation of hydraulics and hydraulic-related phenomena in estuaries, coastal waters and seas. It can be applied to any two-dimensional free-surface flows where stratification can be neglected.