Model Coupling

Introduction

CMS-Flow and CMS-Wave can be run separately or coupled together using a process called steering. The variables passed from CMS-Wave to CMS-Flow are the significant wave height, peak wave period, wave direction, wave breaking dissipation, and radiation stress gradients. CMS-Wave uses the update bathymetry, water levels, and currents from CMS-Flow. The time interval (constant) at which CMS-Wave is run is called the steering interval. The steering process is as follows:

1. CMS-Wave model is run for the first two time steps (time =

t

and time =

t+\Delta t_{w}

) and the wave information is passed to CMS-Flow.

2. CMS-Flow runs from time =

t

until time =

t+\Delta t_{w}+\Delta t

and interpolates the wave variables from during the simulation

3. CMS-Wave is run again for time =

t+2\Delta t_{w}

and

4. The process is repeated over until the end of the steering simulation.

Prediction of Water Levels and Currents

Because CMS-Wave requieres the water surface elevation at times that are ahead of the hydrodynamics, the water surface elevation and currents. If the steering is relatively small (~<30 min), than the values from the previous time step may be used without significant error. This may be expressed in the following form

      $\eta (x,y,t+\Delta t)=\eta (x,y,t)$

where $\eta$ is the water surface elevation.

However, in many coastal engineering projects it is desirable and common to use relatively large steering intervals of 2-3 hours and 3 hours is especially common since many wave buoy data products are at 3 hour intervals. In cases where the relative surface gradients at any time are much smaller than the mean tidal elevation, a better approximation of water level may be obtained by decomposing the water level into

      $\eta (x,y,t+\Delta t)={\bar {\eta }}(x,y,t+\Delta t)+\eta ^{\prime }(x,y,t)$

where ${\bar {\eta }}$ is the component due to astronomical tides, and $\eta ^{\prime }(x,y,t)$ is the component due to tidal, wave, and wind generated surface gradients and can be approximated as $\eta (x,y,t)-{\bar {\eta }}(x,y,t)$ .

Symbol	Description	Units
$\eta$	Water surface elevation	m

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