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      Weak and strong solutions of the \(3D\) Navier-Stokes equations and their relation to a chessboard of convergent inverse length scales

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          Abstract

          Using the scale invariance of the Navier-Stokes equations to define appropriate space-and-time-averaged inverse length scales associated with weak solutions of the \(3D\) Navier-Stokes equations, an infinite `chessboard' of estimates is displayed in terms of labels \((n,\,m)\) beginning at \((1,\,1)\), which corresponds to the inverse Kolmogorov length \(Re^{3/4}\). These estimates ultimately converge to a finite limit, \(Re^3\), as \(n,\,m\to \infty\), although this limit is too large to lie within the physical validity of the equations for realistically large Reynolds numbers. Moreover, all the known time-averaged estimates for weak solutions can be rolled into one single estimate, labelled by \((n,\,m)\). In contrast, those required for strong solutions to exist can be written in another, the only difference being a factor of 2 in the exponent. This appears to be a generalization of the Prodi-Serrin conditions for \(n\geq 1\).

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          Intermittent turbulence in self-similar cascades: divergence of high moments and dimension of the carrier

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            Study of High–Reynolds Number Isotropic Turbulence by Direct Numerical Simulation

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              Dissipation and enstrophy in isotropic turbulence: Resolution effects and scaling in direct numerical simulations

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                Author and article information

                Journal
                30 March 2018
                Article
                1803.11518
                ac045611-3645-4fea-b8f4-8150d380f01d

                http://arxiv.org/licenses/nonexclusive-distrib/1.0/

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                Custom metadata
                2 tables, no figures
                nlin.CD physics.flu-dyn

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