GLS MIXING: Difference between revisions
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[[N2S2_HORAVG]] | [[N2S2_HORAVG]] | ||
There are parameters in [[ocean.in]] that determine whether [[GLS_MIXING]] implements the turbulence closure options of ''k-kl'', | There are parameters in [[ocean.in]] that determine whether [[GLS_MIXING]] implements the turbulence closure options of ''k-kl'', <math>k-\epsilon</math>, or <math>k-\omega</math> | ||
Parents: [[Vertical Turbulence Closure]] | Parents: [[Vertical Turbulence Closure]] |
Revision as of 19:13, 22 November 2006
Generic Length Scale vertical mixing parameterization
- GLS_MIXING
- Option to activate Generic Length Scale vertical mixing parameterization (Warner et al., 2005) for vertical turbulent mixing of momentum and tracers.
- related = CANUTO_A, CANUTO_B, CHARNOK, CRAIG_BANNER, KANTHA_CLAYSON, K_C2ADVECTION, K_C4ADVECTION, N2S2_HORAVG, ZOS_HSIG, TKE_WAVEDISS
- conflict = BVF_MIXING, MY25_MIXING, LMD_MIXING
- routine = gls_corstep.F, gls_prestep.F, roms.in
Wilkin: Here we would write a more verbose description of the GLS scheme (but not a full algorithm/science description). Basically just enough to help a user with a meaningful choice among the following suboptions:
The following CPP options modify the configuration of the Generic Length-Scale vertical turbulence closure:
CANUTO_A CANUTO_B CHARNOK CRAIG_BANNER KANTHA_CLAYSON K_C2ADVECTION K_C4ADVECTION N2S2_HORAVG
There are parameters in ocean.in that determine whether GLS_MIXING implements the turbulence closure options of k-kl, , or
Parents: Vertical Turbulence Closure