[MITgcm-support] eddy transported by mean flow barotropic gyre
Peng Zhan
peng.zhan at kaust.edu.sa
Wed Feb 26 15:12:55 EST 2014
Hi Yang,
I suppose that you added the eddy by adjusting the wind stress would only
affect the surface/ near-surface current, for which the EKE is not high
enough for propagation. Have you checked how deep is your strong small eddy?
Peng
On Wed, Feb 26, 2014 at 9:47 AM, yang.zhang <yang.zhang at mun.ca> wrote:
> Hi, all
>
> I am using MITgcm barotropic gyre to generate a background mean flow,
> then when the flow is stable, I suddenly add a strong small eddy (with
> radius smaller than Rossby deformation radius) by adjusting wind stress at
> some time point,
>
> I am expecting to see :
> this edyy will be transported by the mean flow and evolves with it.
>
> However, the eddy is just sitting there and distort the local stream for a
> while then the flow field restored back to the previous stable state.
>
> I am using a closed basin , free-slip boundary condition, with the
> horizontal diffusion coefficient Ah=0 for the momemtum equation.
> 500m water depth
> 256x256 horizontal grid.
>
>
> Any suggestion ?
>
> Thank you!
> yang
>
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>
--
Peng ZHAN
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Email: *peng.zhan at kaust.edu.sa <peng.zhan at kaust.edu.sa>*
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