Dear maintainers of GeophysicalFlows.jl:
I was wondering that if some further explanations can be added to
some of the examples, which can be understood by the general
public.
For example, linear rotating shallow water dynamics documents how
the PDEs are formulated. I am trying to understand these equations
by real-world example.
If a glass is half-filled with water, and I can somehow rotate this
glass within its symmetrical line with a constant angular velocity,
are those PDEs still remain valid?
Thank you