663 research outputs found
Remarks on a quasi-linear model of the Navier-Stokes Equations
Dinaburg and Sinai recently proposed a quasi-linear model of the
Navier-Stokes equations. Their model assumes that nonlocal interactions in
Fourier space are dominant, contrary to the Kolmogorov turbulence phenomenology
where local interactions prevail. Their equation corresponds to the linear
evolution of small scales on a background field with uniform gradient, but the
latter is defined as the linear superposition of all the small scale gradients
at the origin. This is not self-consistent.Comment: 4 page
Stabilizing the Long-time Behavior of the Navier-Stokes Equations and Damped Euler Systems by Fast Oscillating Forces
The paper studies the issue of stability of solutions to the Navier-Stokes
and damped Euler systems in periodic boxes. We show that under action of fast
oscillating-in- time external forces all two dimensional regular solutions
converge to a time periodic flow. Unexpectedly, effects of stabilization can be
also obtained for systems with stationary forces with large total momentum
(average of the velocity). Thanks to the Galilean transformation and space
boundary conditions, the stationary force changes into one with time
oscillations. In the three dimensional case we show an analogical result for
weak solutions to the Navier- Stokes equations
From the highly compressible Navier-Stokes equations to the Porous Medium equation - rate of convergence
We consider the one-dimensional Cauchy problem for the Navier-Stokes
equations with degenerate viscosity coefficient in highly compressible regime.
It corresponds to the compressible Navier-Stokes system with large Mach number
equal to for going to . When
the initial velocity is related to the gradient of the initial density, a
solution to the continuity equation- converges to the unique
solution to the porous medium equation [13,14]. For viscosity coefficient
with , we obtain a
rate of convergence of in ; for the solution
converges in . For compactly
supported initial data, we prove that most of the mass corresponding to
solution is located in the support of the solution to the
porous medium equation. The mass outside this support is small in terms of
.Comment: 19 page
Geophysical Fluid Dynamics
The workshop “Geophysical Fluid Dynamics” addressed recent advances in analytical, stochastic, modeling and computational studies of geophysical rotating fluids models. Of particular interest on the analytical and stochastic sides were the contributions concerning dispersive mechanism, regularity verses finite-time formation of singularities of certain viscous and inviscid geostrophic models, the primitive equations, Boussinesq approximation, boundary layers and fast rotating fluids. Model reductions, based on asymptotic, scaling analysis and variational methods, were presented. In addition, computational investigations were provided in support of the claim that three-dimensional geophysical turbulent flows exhibit two-dimensional features, at small Rosby numbers
Existence of solutions to a two-dimensional model for nonisothermal two-phase flows of incompressible fluids
We consider a thermodynamically consistent diffuse interface model describing
two-phase flows of incompressible fluids in a non-isothermal setting. This
model was recently introduced in a previous paper of ours, where we proved
existence of weak solutions in three space dimensions. Here, we aim at studying
the mathematical properties of the model in the two-dimensional case. In
particular, we can show existence of global in time strong solutions. Moreover,
we can admit slightly more general conditions on some material coefficients of
the system
Global Regularity vs. Finite-Time Singularities: Some Paradigms on the Effect of Boundary Conditions and Certain Perturbations
In light of the question of finite-time blow-up vs. global well-posedness of
solutions to problems involving nonlinear partial differential equations, we
provide several cautionary examples which indicate that modifications to the
boundary conditions or to the nonlinearity of the equations can effect whether
the equations develop finite-time singularities. In particular, we aim to
underscore the idea that in analytical and computational investigations of the
blow-up of three-dimensional Euler and Navier-Stokes equations, the boundary
conditions may need to be taken into greater account. We also examine a
perturbation of the nonlinearity by dropping the advection term in the
evolution of the derivative of the solutions to the viscous Burgers equation,
which leads to the development of singularities not present in the original
equation, and indicates that there is a regularizing mechanism in part of the
nonlinearity. This simple analytical example corroborates recent computational
observations in the singularity formation of fluid equations
Higher-Order Global Regularity of an Inviscid Voigt-Regularization of the Three-Dimensional Inviscid Resistive Magnetohydrodynamic Equations
We prove existence, uniqueness, and higher-order global regularity of strong
solutions to a particular Voigt-regularization of the three-dimensional
inviscid resistive Magnetohydrodynamic (MHD) equations. Specifically, the
coupling of a resistive magnetic field to the Euler-Voigt model is introduced
to form an inviscid regularization of the inviscid resistive MHD system. The
results hold in both the whole space \nR^3 and in the context of periodic
boundary conditions. Weak solutions for this regularized model are also
considered, and proven to exist globally in time, but the question of
uniqueness for weak solutions is still open. Since the main purpose of this
line of research is to introduce a reliable and stable inviscid numerical
regularization of the underlying model we, in particular, show that the
solutions of the Voigt regularized system converge, as the regularization
parameter \alpha\maps0, to strong solutions of the original inviscid
resistive MHD, on the corresponding time interval of existence of the latter.
Moreover, we also establish a new criterion for blow-up of solutions to the
original MHD system inspired by this Voigt regularization. This type of
regularization, and the corresponding results, are valid for, and can also be
applied to, a wide class of hydrodynamic models
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