[MITgcm-support] 回复: Convection experiment!
Jean-Michel Campin
jmc at ocean.mit.edu
Tue Mar 15 23:16:48 EDT 2011
Hi Antony,
3 remarks:
1) The convection set-up used in the Ocean-Modelling 2011 paper you mentionned
(super-parameterization ...) is somehow similiar to the tutorial_deep_convection
example, but resolution, domain size and parameters are different.
So I don't expect results to be the same.
2) tutorial_deep_convection has been integrated forward for much longer
than the 3 iterations provided in the short test. And it does develop
convective plumes.
So I don't know if the problem you mentionned is because you pick
different parameter/forcing/too-short integration
or if there is a problem in getting MITgcm compiling/running
tutorial_deep_convection example on your computer.
3) the ridgid-lid option normally works fine. Again, unless we got more
details, I would not be able to give any helpfull comments. sorry.
Cheers,
Jean-Michel
On Tue, Mar 15, 2011 at 10:44:23AM +0800, Ertyy wrote:
> In addition, I want to modeling the convection process under leads of sea ice, and since the ocean is mostly covered by sea ice, a rigid-lid is reasonable. However, it is unstable when the rigidlid is turned on.
>
> --- 11年3月15日,周二, Ertyy <antonypolar at yahoo.com.cn> 写道:
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> 发件人: Ertyy <antonypolar at yahoo.com.cn>
> 主题: [MITgcm-support] Convection experiment!
> 收件人: mitgcm-support at mitgcm.org
> 日期: 2011年3月15日,周二,上午9:56
>
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>
>
> Dear All:
> I have tried the deep ocean convection example, however, I did not get what I expected (The only change is that the initial data is not used). The results should be the same with the the NH one presented in JM Campin's paper <Super-parameterization in Ocean Modelling: Application to Deep Convection>.
> My results show a strong horizontal motion of the initial localized cooling disk, which is distorted significantly after several hours, in the meantime, the vertical convection process is not clear. I have no idear what happened. Based on the free surface data, it seems that the gravity waves play a role in the horizontal motion.
> Similar phenomenon happend when I configure a 1D experiment based on the gravity plume experiment, in which the Qnet forcing with a radius of 10 grid is moved to the center of the domain and the bottom is flat.
>
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