I am trying to run an idealized test, only having free surface as the boundary condition to drive the water current inside of my domain. The initial conditions are constant all over the domain:
Code: Select all
u0=0;
v0=0;
temp0=10;
salt0=10;
zeta0=0;
However, I found that the simulated 'zeta' inside of my domain are always around 0 (~10^(-18)). It seems the boundary free surface didn't influence the inner water level at all... I suspected that my CPP option in the header file may have problem, so I used UPWELLING case CPP options ( but #undef ANA_GRID/ #undef ANA_INITIAL/ #define GLS_MIXING). Unfortunately, this doesn't work. I plotted the time-series of simulated free surface on boundary cell and inner cell:
(sorry for the inconvenience. It seems there is a problem of PHP installation on the forum. So I attached URL instead)
https://drive.google.com/open?id=1lNY4v ... exzJFHo18_
The boundary and initial condition files I used are:
https://drive.google.com/open?id=15EFJ6 ... DxaxW9QOWV
https://drive.google.com/open?id=1KmIGy ... q591sauSE2
I have thought the barotropic item ∂η/∂x would work at least....Please let me know if you have any idea. Thanks for your attention!
Best regards
Yifan