Dear all,
I am postprocessing turbulent channel flow data from a 3D1H simulation, in
which I used a coordinate mapping to impose a waviness on the bottom wall
and specified  NUMMODES="9" TYPE="GLL_LAGRANGE_SEM" in inhomogeneous
directions. To analyze the data, I calculate the gradient (FieldConvert -m
mapping -m gradient) of instantaneous fields and write the output in vtu
format.
After the conversion to physical coordinates in Paraview, I extract a
horizontal plane from the resulting vtk fields where I see some spurious
peaks on element borders in the streamwise derivative fields (u_x, v_x,
w_x). I attached a figure showing an example of this, where on the left the
problematic "u_x" is shown and on the right "u_x" derived from the
continuity equation is shown, i.e., "-v_y-w_z". It can be seen that the
fields are the same except some artifacts on element borders in direct
"u_x".
Is this maybe a bug?
Thanks for any feedback.
Regards,
Asim