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Data assimilation for the barotropic Navier-Stokes system

Eduard Feireisl

Abstract

We consider a continuous data assimilation method for the barotropic Navier--Stokes system. The observed solution is supposed to be bounded on the whole time period of observation, while the synchronized solution, usually provided by a numerical method, belongs to the class of dissipative solutions that is considerably larger than the class of conventional weak solutions. A complete synchronization is shown on any compact prediction interval provided the nudging parameters are chosen appropriately.

Data assimilation for the barotropic Navier-Stokes system

Abstract

We consider a continuous data assimilation method for the barotropic Navier--Stokes system. The observed solution is supposed to be bounded on the whole time period of observation, while the synchronized solution, usually provided by a numerical method, belongs to the class of dissipative solutions that is considerably larger than the class of conventional weak solutions. A complete synchronization is shown on any compact prediction interval provided the nudging parameters are chosen appropriately.
Paper Structure (12 sections, 2 theorems, 74 equations)

This paper contains 12 sections, 2 theorems, 74 equations.

Key Result

Theorem 2.2

Let $\Omega \subset R^3$ be a bounded domain of class $C^4$. Let the pressure--density equation of state $p=p(\varrho)$ satisfy the hypotheses S4a, S4A, together with the growth restriction SS3a, where $\gamma > \frac{6}{5}$. Suppose the observed solution $(r, {\bf U})$ belongs to the regularity cla Let $(\varrho, {\bf u})$ be a dissipative solution of the synchronized system S1--S3 in the sense o

Theorems & Definitions (6)

  • Definition 2.1: Dissipative solution
  • Theorem 2.2: Synchronization for the compressible Navier-Stokes system
  • Remark 2.3
  • Proposition 3.1: Conditional regularity
  • Remark 4.1
  • Remark 5.1