A Data Assimilation Algorithm for the Subcritical Surface Quasi-Geostrophic Equation
In this article, we prove that data assimilation by feedback nudging can be achieved for the three-dimensional quasi-geostrophic equation in a simplified scenario using only large spatial scale observables on the dynamical boundary. On this boundary, a scalar unknown (buoyancy or surface temperature...
Saved in:
Published in | Advanced nonlinear studies Vol. 17; no. 1; pp. 167 - 192 |
---|---|
Main Authors | , , |
Format | Journal Article |
Language | English |
Published |
De Gruyter
01.02.2017
|
Subjects | |
Online Access | Get full text |
ISSN | 1536-1365 2169-0375 |
DOI | 10.1515/ans-2016-6019 |
Cover
Summary: | In this article, we prove that data assimilation by feedback nudging can be achieved for the three-dimensional quasi-geostrophic equation in a simplified scenario using only large spatial scale observables on the dynamical boundary. On this boundary, a scalar unknown (buoyancy or surface temperature of the fluid) satisfies the surface quasi-geostrophic equation. The feedback nudging is done on this two-dimensional model, yet ultimately synchronizes the streamfunction of the three-dimensional flow. The main analytical difficulties are due to the presence of a nonlocal dissipative operator in the surface quasi-geostrophic equation. This is overcome by exploiting a suitable partition of unity, the modulus of continuity characterization of Sobolev space norms, and the Littlewood–Paley decomposition to ultimately establish various boundedness and approximation-of-identity properties for the observation operators. |
---|---|
ISSN: | 1536-1365 2169-0375 |
DOI: | 10.1515/ans-2016-6019 |