Hello,
I am not a specialist about advection schemes, but I will try to answer your questions.
For more accurate answers I recommend you check the PhD thesis by Sara Pavan:
www.theses.fr/2016PESC1011.
- it seems to me that the classical PSI scheme implemented in TELEMAC is only 1st order in space and time, maybe the best is to check this in the abovementionned work
- if you want to use less diffusive schemes with tidal flats in TELEMAC-3D, you need to choose the PSI advection scheme (or N) and then specify the value of the option for the advection scheme: SCHEME OPTION FOR ADVECTION OF TRACERS = 4. Without tidal flats, the scheme option 1 is the classical explicit PSI scheme, option 2 is the first-order predictor-corrector and option 3 is the second-order predictor-corrector. I think the PSI scheme with option 4 is second-order but I'm not sure. Again, I recommend you check this in S. Pavan's PhD thesis.
Maybe Sara will improve my answer when she's back from holidays :)
Best regards,
Agnès