Global regularity in two dimensions (Ladyzhenskaya)
Statement
In two space dimensions, for every smooth divergence-free initial velocity with finite energy, the Navier–Stokes equations have a unique solution that stays smooth for all time — no blow-up ever occurs, in contrast with the open 3D case.
Why is it true?
Vorticity in 3D obeys , and the term can amplify vorticity through stretching. In 2D vorticity is a scalar perpendicular to the plane of motion, so that stretching term vanishes identically, leaving only transport and diffusion — nothing left to amplify it without bound.
Proof sketch
Write the vorticity (a scalar in 2D) as and substitute the momentum equation into . Because is divergence-free and two-dimensional, direct computation shows every term coming from that would stretch cancels, leaving the transport-diffusion equation with no source term.
A transport-diffusion equation with no source obeys a maximum principle: along the trajectory of a fluid particle, , and diffusion cannot increase a maximum or decrease a minimum. Hence for all : the vorticity never blows up.
Once vorticity is bounded uniformly in time, elliptic regularity applied to the stream function (recovering from ) bounds all spatial derivatives of in terms of , so stays in every Sobolev space it started in.
Bootstrapping this argument — bounded vorticity gives bounded velocity gradients, which control higher derivatives through the equation itself — shows the solution remains smooth for all , with no finite-time blow-up possible; this is exactly the statement that fails to be known in three dimensions, where the vortex-stretching term is present.
Topics that use this theorem
Step-by-step proofs
No step-by-step proof yet for this theorem.
References
- Charles L. Fefferman (2000). Existence and Smoothness of the Navier-Stokes Equation (Millennium Prize Problem)
- Terence Tao (2016). Finite time blowup for an averaged three-dimensional Navier-Stokes equation · arXiv:1402.0290
- L. Caffarelli, R. Kohn, L. Nirenberg (1982). Partial regularity of suitable weak solutions of the Navier-Stokes equations