Difference between revisions of "INLET TEST CASE"

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This test case models and idealized tidal inlet system. The model domain is a 15x14 km rectangle with a uniform initial depth of 4 m. The model setup parameters are shown in the table below. The domain is separated into two regions: the seaward (top) and back-barrier (bottom) regions. The seaward region is open with radiation conditions on the western, northern and eastern edges. The back-barrier region is enclosed with four walls and is connected to the seaward region through a 2 km wide inlet. The model is forced by a tide and waves. An oscillating water level is imposed on the northern edge with a tidal amplitude of 1 m. Waves are also imposed on the northern edge with a height of 1 m, directed to the south with a period of 10s.
This test case models and idealized tidal inlet system. The model domain is a 15x14 km rectangle with a uniform initial depth of 4 m. The model setup parameters are shown in the table below. The domain is separated into two regions: the seaward (top) and back-barrier (bottom) regions. The seaward region is open with radiation conditions on the western, northern and eastern edges. The back-barrier region is enclosed with four walls and is connected to the seaward region through a 2 km wide inlet. The model is forced by a tide and waves. An oscillating water level is imposed on the northern edge with a tidal amplitude of 1 m. Waves are also imposed on the northern edge with a height of 1 m, directed to the south with a period of 10s.


Files to run this test case can be downloaded here: [[Image:Inlet_test_config.zip]].
Files to run this test case can be downloaded [[media:Inlet_test_config.zip|here]].


Table 1. Important model parameters:
Table 1. Important model parameters:

Revision as of 16:28, 7 January 2009

Inlet Test Case

This test case couples ROMS and SWAN directly using the Modeling Coupling Toolkit (MCT) library. To run this application the user needs to activate INLET_TEST. It only can be run in distributed-memory (MPI) since the parallel threads are split to run both ROMS and SWAN at the same time. This test illustrates the significance of wave-current coupling. This application and coupling methodology is described in Warner et al. (2008).

This test case models and idealized tidal inlet system. The model domain is a 15x14 km rectangle with a uniform initial depth of 4 m. The model setup parameters are shown in the table below. The domain is separated into two regions: the seaward (top) and back-barrier (bottom) regions. The seaward region is open with radiation conditions on the western, northern and eastern edges. The back-barrier region is enclosed with four walls and is connected to the seaward region through a 2 km wide inlet. The model is forced by a tide and waves. An oscillating water level is imposed on the northern edge with a tidal amplitude of 1 m. Waves are also imposed on the northern edge with a height of 1 m, directed to the south with a period of 10s.

Files to run this test case can be downloaded here.

Table 1. Important model parameters:

Model Parameter Variable Value
length, width, depth Xsize, Esize, hmax 15000 m, 14000 m, 4.0 m
number of grid spacings Lm, Mm, N 75, 70, 10
bottom Roughness Zob 0.015 m
time step dt 10 s
simulation steps ntimes 17280 steps (2 days)
morphology factor morph_fac 10 (=20 day scaled simulation)
grain size Sd50 0.10 mm
settle velocity Wsed 11.0 mm s-1
erosion rate Erate 5 x 10-3 kg m-2s-1
critical stress tau_cd, tau_ce 0.10 Nm-2
porosity poros 0.50
bed thickness bed(:, :, :, ithck) 10.0 m
northern edge tide A, Tt 1.0 m, 12 h
northern edge wave height Hsig 2 m
northern edge wave period T 10 s
northern edge wave direction θ from 0° (from North)

Below we provide a brief example of the model output.

Figure 1: ROMS output of free surface and barotropic currents at t=0.5 days.


Figure 2: SWAN output of wave height (Hwave, m) and barotropic currents.