| Type |
Article |
| Date |
2011-11 |
| Language |
English |
| Author(s) |
Simon Guillaume1, Dumas Franck1, Duhaut Thomas1 |
| Affiliation(s) |
1 : IFREMER, DYNECO PHYSED, F-29280 Plouzane, France. |
| Meeting |
15th Biennial Joint Numerical Sea Modelling Group Conference (JONSMOD), Delft, NETHERLANDS, MAY 10-12, 2010 |
| Source |
Ocean Dynamics (1616-7341) (Springer Heidelberg), 2011-11 , Vol. 61 , N. 11 , P. 1887-1903 |
| DOI |
10.1007/s10236-011-0484-6 |
| WOS© Times Cited |
1 |
| Keyword(s) |
Ocean turbulence, Waves, Stokes drift, Iroise sea, MARS, High-frequency radar, OSCR |
| Abstract |
The 1D version of the Model for Applications at Regional Scale is used to parameterize the effects of sea surface waves in 2D in a horizontally homogeneous offshore zone of the Iroise sea. Here we present the first simulation of the Iroise sea including sea surface waves forcing, and more generally, the first study of a boundary layer including the Hasselmann force with a tidal wave. We use a single equation turbulence closure based on a non-local diagnosis for energetic and dissipation length scales. The turbulent energy flux at the surface due to whitecaps and the Hasselmann force induced by Stokes drift are assessed using the whole sea surface waves spectrum given by the Wave Watch Third generation model. The ability of the parameterization to reproduce surface currents over a period of 1 year (2007) is tested with high frequency radar using spectral and time-frequency analysis. One problem with 1D modelling, corresponding to overestimation of current oscillating at inertial frequency is illustrated by comparing 1D and 3D simulations. We found an overall improvement by including the Hasselmann force mainly within the bandwidth of less than one cycle per day to one cycle per day for surface currents. Turbulence is induced by whitecaps decaying rapidly below the ocean surface but the mixed layer below 40 m is deeper due to waves breaking on the sea surface. |
| Full Text |
| File |
Pages |
Size |
Access |
|
17 |
923 KB |
Access on demand |
| Author's final draft |
48 |
36 MB |
Open access |
|
