File:Resuspension.gif

This is a visualization of coupled ROMS-SWAN results for a wave resuspension period. The visualization highlights the sediment export from Poverty Bay, caused by sediment resuspension from Southern Ocean swell waves. Hydrodynamics, sediment-transport, waves, wind, and river discharge are shown.

This visualization contains four main panels showing the currents, sediment-transport, and waves overtop a satellite photograph from World Wind of Poverty Bay and the Waipaoa River flood plain. These panels, from left to right, have the bathymetry contoured every 5 meters from 5 to 45 m and show the:

1) Surface salinity (colors) and surface currents (arrows): The white arrow to the left of the panel is a scale arrow for the currents. This panel also contains the location and travel paths for lagrangian floats initialized every 2 days in the surface waters of Poverty Bay.

2) Fluvial sediment deposition (colors) and bottom currents (arrows): The white arrow to the left of the panel is a scale arrow for the currents. Sediment deposition is shown on a log10 scale in units of kg m-2, with 0, 1, and 2 contoured in grey. When a porosity of ~65% is assumed, these units are equivalent to millimeters of thickness. This panel also contains the location and travel paths for lagrangian floats initialized every 2 days in the bottom waters of Poverty Bay.

3) Depth-integrated fluvial suspended sediment within the water column (colors) and the depth-integrated sediment-transport direction (arrows): The depth-integrated suspended sediment is shown on a log10 scale with 1, 2, and 3 contoured in grey, and is the amount of sediment that would be deposited on the seabed if all the sediment within the water column immediately settled out, with the same units as panel 2. The depth-integrated sediment transport was deemed negligible and the arrows not shown when it was less than 0.04 kg m-1 s-1.

4) Significant wave height: The locations of three current vertical profiles explained below are shown with the stars.