Nonbreaking wave-induced mixing in ROMS?
- jivica
- Posts: 172
- Joined: Mon May 05, 2003 2:41 pm
- Location: The University of Western Australia, Perth, Australia
- Contact:
Nonbreaking wave-induced mixing in ROMS?
Dear ROMS users,
before duplicating already done job I am wondering if someone already did it?
I am looking into the additional mixing (via k-e turbulence) with NONBREAKING(!) waves as additional term in the
shear production term (along with shear and bouy2) as a function of depth, Hs and frequency (Aijaz et. al., 2017; Babanin & Chalikov 2012)
Aijaz, S., M. Ghantous, A. V. Babanin, I. Ginis, B. Thomas, and G. Wake (2017),
Nonbreaking wave-induced mixing in upper ocean during tropical cyclones using coupled hurricane-ocean-wave modeling, J. Geophys. Res. Oceans, 122, 3939–3963, doi:10.1002/ 2016JC012219.
Babanin, A. V., and D. Chalikov (2012), Numerical investigation of turbulence generation in non-breaking potential waves, J. Geophys. Res.,
117, C00J17, doi:10.1029/2012JC007929.
Thanks
Ivica
before duplicating already done job I am wondering if someone already did it?
I am looking into the additional mixing (via k-e turbulence) with NONBREAKING(!) waves as additional term in the
shear production term (along with shear and bouy2) as a function of depth, Hs and frequency (Aijaz et. al., 2017; Babanin & Chalikov 2012)
Aijaz, S., M. Ghantous, A. V. Babanin, I. Ginis, B. Thomas, and G. Wake (2017),
Nonbreaking wave-induced mixing in upper ocean during tropical cyclones using coupled hurricane-ocean-wave modeling, J. Geophys. Res. Oceans, 122, 3939–3963, doi:10.1002/ 2016JC012219.
Babanin, A. V., and D. Chalikov (2012), Numerical investigation of turbulence generation in non-breaking potential waves, J. Geophys. Res.,
117, C00J17, doi:10.1029/2012JC007929.
Thanks
Ivica
Re: Nonbreaking wave-induced mixing in ROMS?
Hi Ivica - Good luck! I stole some code from MOM6 for Langmuir mixing in KPP that I'm playing with. Seems to be an active area of research!
Re: Nonbreaking wave-induced mixing in ROMS?
For wave‐induced vertical mixing in KPP, see Wang et al., JGR 2010, based on Qiao et al, JPO 2004. It is now part of CROCO (ROMS_AGRIF)
Re: Nonbreaking wave-induced mixing in ROMS?
Yes, it's done by Wang et al., JGR 2010 based on Qiao et al, JPO 2004. I added it as a one of the switches (option) for vertical turbulent mixing (lmd_vmix) to the CPP options list (ROMS 3.7), and is running now for the Mid-Atlantic Bight application . To extract wave induced mixing parameter (Bv: m2/s) user need to run the MASNUM model.Please take a look to the attached file.
Cheers,
Farshid
Cheers,
Farshid
- Attachments
-
- bv.pdf
- (19.05 MiB) Downloaded 578 times
Re: Nonbreaking wave-induced mixing in ROMS?
Some of us are too lazy to run a wave model. Check out:
! Li, Q. and B. Fox-Kemper, 2017: Assessing the effects of Langmuir !
! turbulence on the entrainment buoyancy flux in the ocean surface !
! boundary layer, JPO, DOI: 10.1175/JPO-D-17-0085.1 !
! !
! Li, Q., B. Fox-Kemper, Ø. Breivik, and Adrean Webb, 2017: !
! Statistical models of global Langmuir mixing, Ocean Modelling, !
! DOI: 10.1016/j.ocemod.2017.03.016
Re: Nonbreaking wave-induced mixing in ROMS?
Hi Kate, note that nonbreaking-wave-induced mixing and Langmuir turbulence are generally considered two different processes of wave-induced mixing (related to Stokes drift)... Patrick
- jivica
- Posts: 172
- Joined: Mon May 05, 2003 2:41 pm
- Location: The University of Western Australia, Perth, Australia
- Contact:
Re: Nonbreaking wave-induced mixing in ROMS?
Thanks for all responses!
Farhid in which version of ROMS you've implemented it?
Looking in Rutger's version and lmd_vmix.F there is only diffusivity due to the internal waves and not because of surface wind induced waves?
lmd_vmix.F
Patrick,
you have put non-breaking surface wind wave effect into kpp in CROCO? Please if you can point me into which subroutine I should look.
My intention is to put it into gls, it should go into shear production term as addition "W"
\begin{equation}
\ni (M^2 + \alpha N^2) + W
\end{equation}
If you have information about wind induced waves from spectral model (or via coupling) it should be straight forward.
W is simple function of H_S is significant wave height, \omega is peak angular frequency, k is wavenumber, z is depth:
\begin{equation}
W = 0.0014 * k (\frac{\omega H_s}{2) e^{kz})^3
\end{equation}
Thanks!
Ivica
Farhid in which version of ROMS you've implemented it?
Looking in Rutger's version and lmd_vmix.F there is only diffusivity due to the internal waves and not because of surface wind induced waves?
lmd_vmix.F
Code: Select all
! Compute interior diffusivity due to wave breaking (Gargett and
! Holloway.
you have put non-breaking surface wind wave effect into kpp in CROCO? Please if you can point me into which subroutine I should look.
My intention is to put it into gls, it should go into shear production term as addition "W"
\begin{equation}
\ni (M^2 + \alpha N^2) + W
\end{equation}
If you have information about wind induced waves from spectral model (or via coupling) it should be straight forward.
W is simple function of H_S is significant wave height, \omega is peak angular frequency, k is wavenumber, z is depth:
\begin{equation}
W = 0.0014 * k (\frac{\omega H_s}{2) e^{kz})^3
\end{equation}
Thanks!
Ivica
Re: Nonbreaking wave-induced mixing in ROMS?
Dear Ivica,
Please have a look to "lmd_vmix.F " and the section, regarding to "Sum contributions due to internal wave breaking...", in fact non-breaking wave induced coefficient (Bv(i,j,k); (m2/s)) here is used to enhance the vertical mixing for momentum (Akv(i,j,k); (m2/s)) and tracer (Akt(i,j,k); (m2/s)) respectively.
Akv* = Akv + Bv (1)
Akt* = Akt + cBv (2)
where "c" is weighting coefficient of wave‐induced mixing (Yonggang Wang et al. 2010).
Cheers,
Farshid
Please have a look to "lmd_vmix.F " and the section, regarding to "Sum contributions due to internal wave breaking...", in fact non-breaking wave induced coefficient (Bv(i,j,k); (m2/s)) here is used to enhance the vertical mixing for momentum (Akv(i,j,k); (m2/s)) and tracer (Akt(i,j,k); (m2/s)) respectively.
Akv* = Akv + Bv (1)
Akt* = Akt + cBv (2)
where "c" is weighting coefficient of wave‐induced mixing (Yonggang Wang et al. 2010).
Cheers,
Farshid
- Attachments
-
- Yonggang Wang et al 2010.pdf
- (12.2 MiB) Downloaded 548 times
-
- Qiao_et_al-2004-Geophysical_Research_Letters.pdf
- (1.19 MiB) Downloaded 541 times
-
- Posts: 26
- Joined: Wed Jul 19, 2017 4:03 pm
- Location: Zhejiang University
Re: Nonbreaking wave-induced mixing in ROMS?
Do you mean the ROMS 3.7 have included such an option ? I didn't find it.fdaryabor wrote: ↑Fri Jun 01, 2018 3:07 pm Yes, it's done by Wang et al., JGR 2010 based on Qiao et al, JPO 2004. I added it as a one of the switches (option) for vertical turbulent mixing (lmd_vmix) to the CPP options list (ROMS 3.7), and is running now for the Mid-Atlantic Bight application . To extract wave induced mixing parameter (Bv: m2/s) user need to run the MASNUM model.Please take a look to the attached file.
Cheers,
Farshid
Do you mean add such an option and modification to code to your own ROMS code ? If so, could you please send me a copy of the modified code ? joe211010@gmail.com.
What's more, I didn't want to use the MASNUM model. Is it possible to use a ERA5 wave spectrum data product to calculate Bv ?
Thank you very much ! Looking forward to hearing from you soon!