2017
DOI: 10.1007/s00220-017-2846-5
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Existence and Non-uniqueness of Global Weak Solutions to Inviscid Primitive and Boussinesq Equations

Abstract: We consider the initial value problem for the inviscid Primitive and Boussinesq equations in three spatial dimensions. We recast both systems as an abstract Eulertype system and apply the methods of convex integration of De Lellis and Székelyhidi to show the existence of infinitely many global weak solutions of the studied equations for general initial data. We also introduce an appropriate notion of dissipative solutions and show the existence of suitable initial data which generate infinitely many dissipativ… Show more

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Cited by 19 publications
(24 citation statements)
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“…This is the initial energy jump typical for weak solutions obtained through the method of convex integration; see [8,9,19]. Nevertheless, it is possible to remove this drawback by modifying the convex integration scheme as explained in [9,20], at least for certain initial velocity.…”
Section: E(t) > E(0)mentioning
confidence: 99%
“…This is the initial energy jump typical for weak solutions obtained through the method of convex integration; see [8,9,19]. Nevertheless, it is possible to remove this drawback by modifying the convex integration scheme as explained in [9,20], at least for certain initial velocity.…”
Section: E(t) > E(0)mentioning
confidence: 99%
“…For a thorough report of these developments and connections to Nash's work on isometric embeddings, we refer to [25]. Another, somewhat independent strand, was to adapt the techniques to other systems of equations, such as compressible Euler system [13], active scalar equations [10,18,52,53] and others [8,14,15,37]. A key point in the technique is a study of the phase-space geometry of the underlying system, to understand the interaction of high-frequency perturbations with the nonlinearity in the equations in the spirit of L. Tartar's compensated compactness.…”
Section: Introductionmentioning
confidence: 99%
“…One of the main issues is the presence of multiple time-scales, where different processes (e.g., external and internal gravity waves, eddies, biochemical reactions) take different times to be completed. Since the primitive equations arise from hyperbolic conservation laws ( [2,3]), explicit time integrators and Runge-Kutta schemes would hypothetically be good choices for solving it. However, these schemes are not capable of efficiently handling multiple time-scales, because the time-steps restrictions are too severe, resulting in a significant degradation of performance.…”
Section: Introductionmentioning
confidence: 99%