Difference between revisions of "Xlsc0 (surface mixing length scale constant)"
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$\kappa=0.4$ is the von Karman's constant; | $\kappa=0.4$ is the von Karman's constant; | ||
| − | $d_s$ = xlsc0 $\cdot$ ''surface layer thinkness''. | + | $d_s$ = '''xlsc0''' $\cdot$ ''surface layer thinkness''. |
| − | As a scale constant, | + | As a scale constant, '''xlsc0''' should take a value between 0 and 1. Note that the spatially varying option (xlsc.gr3) is disabled in the latest SCHISM version. |
If wind wave module is invoked, the ''surface layer thickness'' is taken as 0.6$H_s$ (significant wave height) following Terray et al. (1996); otherwise, it is taken as the distance between the top two vertical layers. | If wind wave module is invoked, the ''surface layer thickness'' is taken as 0.6$H_s$ (significant wave height) following Terray et al. (1996); otherwise, it is taken as the distance between the top two vertical layers. | ||
Latest revision as of 20:45, 23 May 2018
For the Generic Length Scale (GLS) turbulence closure (Umlauf and Burchard, 2003) in SCHISM, the mixing length ($l$) near the free surface is determined as
$l=\kappa d_s$ (Zhang and Baptista, 2008),
where
$\kappa=0.4$ is the von Karman's constant;
$d_s$ = xlsc0 $\cdot$ surface layer thinkness.
As a scale constant, xlsc0 should take a value between 0 and 1. Note that the spatially varying option (xlsc.gr3) is disabled in the latest SCHISM version.
If wind wave module is invoked, the surface layer thickness is taken as 0.6$H_s$ (significant wave height) following Terray et al. (1996); otherwise, it is taken as the distance between the top two vertical layers.
References:
Terray, E.A., Donelan, M.A., Agrawal, Y.C., Drennan, W.M., Kahma, K.K., Williams, A.J., Hwang, P.A. and Kitaigorodskii, S.A., 1996. Estimates of kinetic energy dissipation under breaking waves. Journal of Physical Oceanography, 26(5), pp.792-807.
Umlauf, L. and Burchard, H., 2003. A generic length-scale equation for geophysical turbulence models. Journal of Marine Research, 61(2), pp.235-265.
Zhang, Y. and Baptista, A.M., 2008. SELFE: a semi-implicit Eulerian–Lagrangian finite-element model for cross-scale ocean circulation. Ocean modelling, 21(3-4), pp.71-96.
