[MITgcm-support] 回复: 回复: barotropic nondivergent run
钱钰坤
qianyk at mail3.sysu.edu.cn
Mon Jul 20 05:53:15 EDT 2015
Hi Ryan,
Thanks very much for your reply and sharing your python QG model. Non-divergent is essential to me, not QG.
I'll try some simulations with and without rigid lid option and then see the differences.
------------------
Best regards
Yu-Kun Qian (钱钰坤)
Center for Monsoon and Environment Research
Department of Atmospheric Sciences
School of Environmental Science and Engineering
Sun Yat-sen University
No. 135 Xingang West Road, Haizhu District
Guangzhou, 510275, P.R. China
Tel; 020-84115227
Email: qianyk at mail3.sysu.edu.cn
------------------ 原始邮件 ------------------
发件de人: "Ryan Abernathey"<ryan.abernathey at gmail.com>;
发送时间: 2015年7月20日(星期一) 中午11:00
收件人: "mitgcm-support at mitgcm.org"<mitgcm-support at mitgcm.org>;
主题: Re: [MITgcm-support]回复: barotropic nondivergent run
Yu-Kun,
You are correct--you can make the MITgcm into a 2D, non-divergent barotropic model by using only one vertical level and a rigid lid. You can also use a cartesian geometry. However, you can't make it formally "quasigeostrophic" because it is at its core a primitive equation model. In practice you might find a configuration that obeys QG dynamics to a good approximation, but it will not be exact.
If you really want to to QG simulations, you should probably use a different model. If you can live with doubly-periodic boundary conditions, I will humbly suggest the python-based QG model I have been developing along with a few other people, pyqg:
https://github.com/rabernat/pyqg
If you want sidewalls or bottom bathymetry, you will need something else for now.
Best,
Ryan
On Sun, Jul 19, 2015 at 10:27 PM, 钱钰坤 <qianyk at mail3.sysu.edu.cn> wrote:
Hi Matt,
Thanks for your reply but it seems a little odd to me that the model is always non-divergent, at least for horizontal non-divergent (not 3D non-divergent).
For atmosphere simulation, horizontal non-divergent model may limit the evolution of synoptic systems. For non-hydrostatic simulation in the ocean, non-divergent dynamics is also improper.
I can find a pre-defined momentum diagnostic monHDIV representing the horizontal divergence.
As I see, in a barotropic model described by three variables (u, v, h), free surface (h) variations are caused by mass convergence/divergence. When the non-divergence constrain is put, the model can be reduced to only a single variable streamfunction. Then how can I used MITgcm to mimic such dynamics?
------------------
Best regards
Yu-Kun Qian (钱钰坤)
Center for Monsoon and Environment Research
Department of Atmospheric Sciences
School of Environmental Science and Engineering
Sun Yat-sen University
No. 135 Xingang West Road, Haizhu District
Guangzhou, 510275, P.R. China
Tel; 020-84115227
Email: qianyk at mail3.sysu.edu.cn
------------------ 原始邮件 ------------------
发件de人: "Matthew Mazloff"<mmazloff at ucsd.edu>;
发送时间: 2015年7月18日(星期六) 凌晨3:42
收件人: "mitgcm-support"<mitgcm-support at mitgcm.org>;
主题: Re: [MITgcm-support] barotropic nondivergent run
Hi Yu-Kun
The MITgcm is always non-divergent
Matt
On Jul 17, 2015, at 1:28 AM, 钱钰坤 <qianyk at mail3.sysu.edu.cn> wrote:
Hi all,
I want to investigate the wind-driven ocean dynamics using QG barotropic nondivergent setup of MITgcm. So far as I know, QG (quasi-geostrophic) means using Cartesian coordinates with f0 and sbeta set in parameter file 'data' to mimic beta-plane approximation. Barotropics means that only one single layer is used in the model. I've no idea how to constrain the model to produce nondivergent flow.
I guess using the rigid lid option to force the flow nondivergent but I'm not sure. Can anyone give some suggestions? Many thanks in advance.
------------------
Best regards
Yu-Kun Qian (钱钰坤)
Center for Monsoon and Environment Research
Department of Atmospheric Sciences
School of Environmental Science and Engineering
Sun Yat-sen University
No. 135 Xingang West Road, Haizhu District
Guangzhou, 510275, P.R. China
Tel; 020-84115227
Email: qianyk at mail3.sysu.edu.cn
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