Hello,
In term of velocity, the unstationnary open boundaries (forced by a tidal signal for instance) are treated with the Thompson method in Telemac.
Is there currently a way of dealing with this type of boundary condition for a tracer flux?
Indeed, an open boundary should allow the perturbations generated inside the computational domain to leave it without deterioration of the inner model solution (made possible in Telemac with the flag "4=FREE TRACER" in the .cli file). However, there is sometimes competing requirement that physically important information be conveyed inwards (if not my salinity plume dissipate with no limit).
Thank you for indicating me how I should deal with this BC issue.
Best regards,
Alexis