Reduced Order Models for the Quasi-Geostrophic Equations: A Brief Survey

dc.contributor.authorMou, Changhongen
dc.contributor.authorWang, Zhuen
dc.contributor.authorWells, David R.en
dc.contributor.authorXie, Xupingen
dc.contributor.authorIliescu, Traianen
dc.contributor.departmentMathematicsen
dc.date.accessioned2021-01-08T15:50:29Zen
dc.date.available2021-01-08T15:50:29Zen
dc.date.issued2020-12-31en
dc.date.updated2021-01-08T14:48:13Zen
dc.description.abstractReduced order models (ROMs) are computational models whose dimension is significantly lower than those obtained through classical numerical discretizations (e.g., finite element, finite difference, finite volume, or spectral methods). Thus, ROMs have been used to accelerate numerical simulations of many query problems, e.g., uncertainty quantification, control, and shape optimization. Projection-based ROMs have been particularly successful in the numerical simulation of fluid flows. In this brief survey, we summarize some recent ROM developments for the quasi-geostrophic equations (QGE) (also known as the barotropic vorticity equations), which are a simplified model for geophysical flows in which rotation plays a central role, such as wind-driven ocean circulation in mid-latitude ocean basins. Since the QGE represent a practical compromise between efficient numerical simulations of ocean flows and accurate representations of large scale ocean dynamics, these equations have often been used in the testing of new numerical methods for ocean flows. ROMs have also been tested on the QGE for various settings in order to understand their potential in efficient numerical simulations of ocean flows. In this paper, we survey the ROMs developed for the QGE in order to understand their potential in efficient numerical simulations of more complex ocean flows: We explain how classical numerical methods for the QGE are used to generate the ROM basis functions, we outline the main steps in the construction of projection-based ROMs (with a particular focus on the under-resolved regime, when the closure problem needs to be addressed), we illustrate the ROMs in the numerical simulation of the QGE for various settings, and we present several potential future research avenues in the ROM exploration of the QGE and more complex models of geophysical flows.en
dc.description.versionPublished versionen
dc.format.mimetypeapplication/pdfen
dc.identifier.citationMou, C.; Wang, Z.; Wells, D.R.; Xie, X.; Iliescu, T. Reduced Order Models for the Quasi-Geostrophic Equations: A Brief Survey. Fluids 2020, 6, 16.en
dc.identifier.doihttps://doi.org/10.3390/fluids6010016en
dc.identifier.urihttp://hdl.handle.net/10919/101803en
dc.language.isoenen
dc.publisherMDPIen
dc.rightsCreative Commons Attribution 4.0 Internationalen
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/en
dc.subjectreduced order modelsen
dc.subjectquasi-geostrophic equationsen
dc.subjectclosure modelsen
dc.titleReduced Order Models for the Quasi-Geostrophic Equations: A Brief Surveyen
dc.title.serialFluidsen
dc.typeArticle - Refereeden
dc.type.dcmitypeTexten

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