[MITgcm-support] 3D interpolation of model state by flt floats
钱钰坤
qianyk at mail3.sysu.edu.cn
Sun Mar 29 11:06:11 EDT 2020
Hi Paola,
I understand it better now. Maybe we need an interpolation function to handle the case of land points.
Thank you very much for your quick reply.
------------------
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 ------------------
发件人: "Paola Cessi"<pcessi at ucsd.edu>;
发送时间: 2020年3月29日(星期天) 晚上10:53
收件人: "mitgcm-support"<mitgcm-support at mitgcm.org>;
主题: Re: [MITgcm-support] 3D interpolation of model state by flt floats
Hi,
the FLT package as it is now interpolates all fields using neighboring points, including land points. This is OK for velocities which are indeed zero on the boundaries, but not for T,S, tracers and SSH, which are set to zero on the land points, which is not their true value. So for T, S, tracers and SSH it is better not to interpolate at all and just use the value on the grid at the nearest cell point, i.e. using NINT in all three directions.
Paola
----------------------------------------------
Paola Cessi
Scripps Institution of Oceanography
9500 Gilman Drive #0213
La Jolla, CA 92093-0213
USA
Tel: +1 858 534 0622 Fax: +1 858 534 8045
e-mail: pcessi at ucsd.edu Web: http://www-pord.ucsd.edu/~pcessi
Delivery address (Fed-Ex, DHL, UPS, etc.):
Paola Cessi
University of California San Diego
Keck Center - Room 366
8851 Shellback Way
La Jolla, CA 92093-0213
USA
On Mar 29, 2020, at 7:42 AM, 钱钰坤 <qianyk at mail3.sysu.edu.cn> wrote:
Hi all,
When I tried to sample the model state using 3D floats (flt pkg), I found that the sampled fields are not smooth (like a step funtion in some way) as I expected (I made a comparison with the offline-sampled results). When I looked into flt_traj.F, there are some codes doing the interpolation of model state by floats. For a 3D type float (not horizontal 2D float), I would expect a trilinear (x, y, z) interpolation of the model state. However, I found the following lines (https://github.com/MITgcm/MITgcm/blob/master/pkg/flt/flt_traj.F#L134):
CALL FLT_BILINEAR (ix,jy,uu,uVel, kp,1,bi,bj,myThid)
CALL FLT_BILINEAR (ix,jy,vv,vVel, kp,2,bi,bj,myThid)
CALL FLT_BILINEAR2D(ix,jy,pp,etaN, 0,bi,bj,myThid)
CALL FLT_BILINEAR (ix,jy,tt,theta, kp,0,bi,bj,myThid)
CALL FLT_BILINEAR (ix,jy,ss,salt, kp,0,bi,bj,myThid)
For a 3D linear interpolation, I think FLT_TRILINEAR would be much better, with proper vertical position kp. Here kp is a roundoff of the vertical position (https://github.com/MITgcm/MITgcm/blob/master/pkg/flt/flt_traj.F#L106):
kp = NINT(kpart(ip,bi,bj))
When I change FLT_BILINEAR(...) to FLT_TRILINEAR(ix,jy,kpart(ip,bi,bj),tt,theta,0,bi,bj,myThid), I got almost identical results both online and offline. No step-funciton-like behavior.
Shouldn't it be changed to FLT_TRILINEAR?
------------------
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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