As a student of meteorology, I wonder why Navier-Stokes equations (NSE) are still not understood in terms of whether or not there are unique solutions. In atmospheric dynamics, NSE is used as a basic equation of motion governing the dynamic behavior of air parcels, taught from the first lecture on and included (in direct or modified form) in numerical prediction algorithms.
Assuming the atmosphere can be modeled by NSE, we know there ARE solutions because when we look out the window there is SOME weather. What I mean: IF a physical solution exists for all times and for the whole field, there IS a solution, even if we don't know it.
So what is the mathematical problem in practical terms? From a naïve point of view, I am tempted to assume that atmospheric motion for some spherical Earth model can be predicted spatially and for all time with arbitrary precision if we know the starting conditions with arbitrary precision. Is there a point at which a numerical prediction based on some initial solution necessarily fails or suddenly becomes ambiguous?
I've never tried: but does it really mean we have not one known solutions for $u(x,t)$ and a given $p(x,t)$ and $\nu>0$? Not even some trivial ones? Hard to believe; can someone shed some light on it without going into deep maths?