**not**claiming any major breakthrough on this problem, which remains extremely challenging in my opinion.)

This problem is formulated in a qualitative way: the conjecture asserts that the velocity field stays smooth for all time, but does not ask for a quantitative bound on the smoothness of that field in terms of the smoothness of the initial data. Nevertheless, it turns out that the compactness properties of the periodic Navier-Stokes flow allow one to equate the qualitative claim with a more concrete quantitative one. More precisely, the paper shows that the following three statements are equivalent:

- (Qualitative regularity conjecture) Given any smooth divergence-free data , there exists a global smooth solution to the Navier-Stokes equations.
- (Local-in-time quantitative regularity conjecture)

Given any smooth solution to the Navier-Stokes equations with , one has the*a priori*bound for some non-decreasing function . - (Global-in-time quantitative regularity conjecture) This is the same conjecture as 2, but with the condition replaced by .

It is easy to see that Conjecture 3 implies Conjecture 2, which implies Conjecture 1. By using the compactness of the local periodic Navier-Stokes flow in , one can show that Conjecture 1 implies Conjecture 2; and by using the energy identity (and in particular the fact that the energy dissipation is bounded) one can deduce Conjecture 3 from Conjecture 2. The argument uses only standard tools and is likely to generalise in a number of ways, which I discuss in the paper. (In particular one should be able to replace the norm here by any other subcritical norm.)

When I previously discussed the Navier-Stokes equations, I suggested that perhaps the best hope to attack this equation was by what I called “Strategy 1″: by obtaining a new a priori bound on solutions to this equation. What this result indicates (in the periodic case) is that this strategy is in fact essentially the *only* strategy for solving this equation, since the regularity problem is in fact *equivalent* to that of obtaining an a priori bound.

As the qualitative result is now logically equivalent to a quantitative one, it seems to me that purely “soft” approaches to the problem are now extremely unlikely to work, and that a substantial amount of “hard analysis” would have to go into any putative proof of this problem. In particular, it is clear that if one attempts to construct solutions by expressing them as the limit of some sort of regularised (or discretised) solutions, this can only work if one can obtain a priori bounds on the approximating solutions which are uniform in the approximation parameter, since all other bounds will be lost in the passage to the limit. One of course has the energy inequality for such approximate solutions (which is how Leray constructed global weak solutions to the Navier-Stokes equations), but to obtain smooth solutions one needs to control a norm such as H^1. [Incidentally, the energy inequality does show that is square-integrable in time, but this is quite far away from what we really need, which is that is bounded. Actually, these two statements are radically different: the former is a supercritical control on u and the latter is subcritical control.]

One amusing consequence of this equivalence is that the Navier-Stokes regularity conjecture is also equivalent to a non-perturbative global stability result for the Navier-Stokes flow. In particular, if the Navier-Stokes regularity conjecture is true, then the solution map maps any bounded set in to a bounded set in in a Lipschitz manner, if one fixes the mean velocity to avoid issues with drift. (The dissipation is what allows one to control things at very late times; this is one of the strange features of supercritical estimates such as the energy inequality, in that they offer very poor short-time control but give excellent long-time control.)

## 19 comments

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10 October, 2007 at 1:49 pm

neurooneDear terry,

I am not a maths or physics major student,my interest is to crack the mystery of the brain or the neurosystem by mathematical ways.

I think neuroscience have the same terminal goal with maths, and the cognition of human being infulence the way human do maths, they are two interacting things.

what I want to ask is that, do you have any interest on neuroscience? do you think maths is an effective way to decipher the code of the cognition?

10 October, 2007 at 4:19 pm

IU studentHi Prof. Tao,

As I know , the uniqueness of weak solutions is false for Euler equation.

How about N-S equation ? Is the weak solution unique ?

What is the connection between the Hausdorff dimension of singular set of a suitable weak sloution and the regularity ?

14 October, 2007 at 5:25 pm

Terence TaoDear IU student,

I do not know of rigorous non-uniqueness results for the Navier-Stokes equation, but I would not be surprised if weak solutions are indeed non-unique here. On the other hand there are various “weak-strong uniqueness theorems” which assert that if a sufficient amount of regularity is assumed on the weak solution, then the weak solution is in fact unique. I am not sure exactly what the minimal amount of regularity is in the literature in order to obtain this uniqueness result, but I would expect that one needs to control the weak solution in either a sub-critical or critical norm in order for the known methods for establishing uniqueness to be effective.

I am not sure as to the thrust of your second question; a solution is regular if and only if its singular set is empty. There are various upper bounds on the dimension of the singular set to a weak or strong solution to the Navier-Stokes equations, in particular a well-known result of Caffarelli, Kohn, and Nirenberg, though again the bounds here are subcritical or critical in nature.

17 October, 2007 at 11:26 pm

Shuanglin ShaoTwo more typos?

(1) On page 7, line 3, “A^2″ instead of “A” or using bound 1 by suppressing A;

(2) On page 9, subsection 3.1, “from” instead of “implies”.

18 October, 2007 at 6:25 am

Terence TaoDear Shuanglin,

Thanks for the corrections!

2 January, 2008 at 4:09 pm

DavePurvanceBound for Periodic Navier-Stokes EquationI have shown that a for any spatially periodic flow of initial finite value the incompressible Navier-Stokes equation can be posed as a nonlinear matrix differential equation

(1)

where matrix is principally a function of wavenumber-shifted . When is assumed to be the time series

(2),

then (1) becomes

(3)

where are matrices made from . Matching coefficients in (3) when solves for the unknown flow coefficients in (3). For they are

. (4)

The remarkable discovery I have recently made is that the only difference between in (4) and made from the Taylor expansion of the matrix exponential

(5)

i.e.,

(6)

is a left-to-right reversal in the order of matrix products in some of the terms making up and . When commute, the order of a matrix product is immaterial and coefficients become , as they must.

What I have argued here is that magnitude of the difference between and

(7)

is bounded by the magnitude of . The Navier-Stokes are stable and therefore coefficients converge, implying that converge.

Care to comment?

9 May, 2009 at 4:32 pm

StudentI believe the integral in the middle of Page 5 is missing dt.

I could not figure out how you derived the 2nd to last inequality on the bottom of page 6; if you could give hints, it will be great.

On page 9, you state “The least non-trivial eigenvalue of −(Laplace) on the torus is 1″ I’m sory if it’s a poor question, but I don’t see what you are trying to say by that.

Finally, on this same page you have an epsilon depending on M, but I guess you mean on E.

9 May, 2009 at 5:03 pm

Terence TaoThanks for the corrections! For the inequality, one can use Holder’s inequality to bound the norm of by the norm of u and the norm of , which by another application of Holder’s inequality can be interpolated between the and norms of . Meanwhile, T can be replaced by by definition of T.

The decay of for a function u of mean zero is controlled by the least non-trivial eigenvalue of the Laplacian. This can be seen by expanding u into eigenfunctions of the Laplacian and using functional calculus. (The mean zero condition is needed to ensure that u has no coefficient corresponding to the trivial eigenvalue of 0, or the trivial eigenfunction of 1.)

12 May, 2009 at 11:40 am

PDEbeginnerDear Prof. Tao,

I can’t derive the inequality in Lem 2.1. I tried in the following way:

for some

constants , where and we use the Einstein’s notation for the summations and omit the

t in u and F.

On the other hand, the heat equation in the proof seems to be

.

12 May, 2009 at 12:03 pm

Terence TaoDear PDEbeginner,

The right-hand side of that inequality should be rather than ; sorry about that. (By the way, in your computation, the term should be a .)

20 May, 2009 at 6:52 pm

StudentOn page 1, you state “as is well-known, we can use Leray projections to eliminate the pressure p.” I clearly see the benefit of utilizing this projection but what is the cost of doing this?

On top page 5, you state “if u0 is divergence-free then a strong H10 solution u of (4) must be divergence-free also.” I”m sorry I do not see this. Please explain.

On middle of page 9, you state “T′ ≤ 1 / epsilon” but your initial supposition was 0 ≤ T’ ≤ 1/epsiolon^2.”

On top page 10, you state “Suppose for contradiction that Conjecture 1.2 failed” when you mean Conjecture 1.3.

Finally, while reading your paper with much interest, I came across a paper “Global well-posedness for the critical 2D dissipative quasi-geostrophic equation (QG)” by A. Kiselev, F. Nazarov, A. Volberg (The paper is readily found on Arxiv). Some such as Peter Constantin have paid much attention to this QG, which is in principle supposed to be a toy model for the Euler Equation. The 2D critical dissipative QG case had a breakthrough in 2006 by the work shown in this paper. In particular, these three authors gave a brilliant proof constructing a moduli of continuity which works very much like your “non-decreasing function F.” Their method was continued to the case of super-critical QG (cf. Xinwei Yu) with the cost of initial data being small. I am investigating why this method cannot be applied to the NSE, although I’m guessing the main reason is the pressure term that exists in the NSE but not QG. I would be curious to know if you have any thought on this regard.

Thank you very much.

21 May, 2009 at 9:51 am

Terence TaoDear Student,

The main drawback of applying the Leray projection is that the resulting evolution equation for the velocity field u is non-local. But for Fourier-based techniques, the projection is fairly harmless.

If the initial data is divergence free, then so is the linear solution (note that divergence commutes with Fourier multipliers such as ), and so is the integral term involving D, thanks to the nature of D. One can justify these computations in a distributional sense (testing (4) against some spacetime test function).

As for QG, one can use perturbation theory (at least in principle) to obtain global well-posedness for supercritical equations (such as Navier-Stokes in 3D) provided that some critical norm of the data is small. It seems that the result of Yu you mention is in this category. There are similar results known for Navier-Stokes, e.g. global well-posedness if the H^{1/2} norm of the velocity is small (a result due, if I recall correctly, to Kato). However these results are not enough to deal with the non-perturbative setting for large data, as I discuss in my post

https://terrytao.wordpress.com/2007/03/18/why-global-regularity-for-navier-stokes-is-hard/

Thanks for the corrections!

24 May, 2009 at 2:22 am

PDEbeginnerDear Prof. Tao,

This paper is very clear for $H^1$ theory for the local wellposedness, I like it very much!

As for the derivation of Conjecture 1.2 from Conjecture 1.3, it seems a bootstrap argument is enough: On each time interval , we take as the initial data, apply Conjecture 1.3, and then obtain a uniform bounds for on , where can arbitrarily large. Of course, the argument for controlling the at large time is very nice, I like it very much!

24 May, 2009 at 9:08 am

Terence TaoDear PDEBeginner,

The bound obtained by applying Conjecture 1.3 iteratively is not uniform in N, because the H^1 norm of u(n) is not conserved in n. Each application of Conjecture 1.3 can control the H^1 norm of u(n+1) in terms of the H^1 norm of u(n), but the former can be much larger than the latter, and so one ends up with a growth in N. This is why one needs the large time estimate as well.

28 May, 2009 at 7:23 pm

StudentDear Professor Tao:

There is something about NSE being critical (sub or super) that I do not understand and I would really appreciate if you could clarify.

On one hand we have Quasi-geostrophic Equation (QG) which is a toy model for 3-D NSE and is critical with power of Laplacian at 1/2, subcritical if larger than 1/2 and supercritical if less than 1/2. That is, if \theta (x, t) is a solution to QG, then so is \theta (Cx, Ct) for any C a real number.

I tried to see what is the power of Laplacian of dissipative NSE such that same result occurs. First, I took Leray’s Projector to replace the NSE in a similar setting to the QG, in R^n so that the Projector commutes with Laplacian and hence the Projector really only affects the nonlinear term. Then, the power of Laplacian such that the equation enjoys a nice scaling with no multiplication by some constant seems to be 1/2 as well (and this is the case even if I do not take the Leray Projector; i.e. with the power at 1/2, if u(x, t) and p(x, t) solves the NSE, then so does u(Cx, Ct) and p(Cx, Ct)).

Is this correct? And if so, I am very confused because adding more power of Laplacian should make any PDE easier to work with and hence any more power on the Laplacian than 1/2 should be subcritical rather than supercritical. In particular, the power at 1 should be subcritical, not super, but I know that’s false.

I know the dissipative NSE is solved for the powe bigger than 5/4 (by Jonathan Mattingly). But what is the power that separates super and subcritical for NSE?

Moreover, I did read your notes on the issues of critical (sub, super) in the link below, but I guess you are talking about quantities (e.g. energy) and not the equation.

https://terrytao.wordpress.com/2007/03/18/why-global-regularity-for-navier-stokes-is-hard/

How are they related?

Thank you.

29 May, 2009 at 7:41 am

Terence TaoDear student,

Equations, in and of themselves, are neither critical, subcritical, or supercritical. In order to obtain such a classification one needs both an equation and some functional (such as the energy, the mass, or maybe a Sobolev norm). Basically, both equations and functionals are naturally associated with a means to rescale the solution. If the two rescalings match, the functional is critical for the equation; otherwise, they are supercritical or subcritical depending on which rescaling is stronger at finer scales. When one says a statement such as “Navier-Stokes is supercritical in three dimensions”, this is shorthand for “The strongest known controlled quantity for Navier-Stokes, namely the energy, is supercritical for that equation in three dimensions.”

In the case of Navier-Stokes in d dimensions, for instance, the rescaling that preserves the equation is given by , while the rescaling that preserves the energy is . In three and higher dimensions, the energy rescaling is more severe at fine scales , hence the energy is supeercritical for the equation in that setting.

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