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Global Stability of Fluid Flows Despite Transient Growth of Energy
Indexado
WoS WOS:000807220600001
Scopus SCOPUS_ID:85131464020
DOI 10.1103/PHYSREVLETT.128.204502
Año 2022
Tipo artículo de investigación

Citas Totales

Autores Afiliación Chile

Instituciones Chile

% Participación
Internacional

Autores
Afiliación Extranjera

Instituciones
Extranjeras


Abstract



Verifying nonlinear stability of a laminar fluid flow against all perturbations is a central challenge in fluid dynamics. Past results rely on monotonic decrease of a perturbation energy or a similar quadratic generalized energy. None show stability for the many flows that seem to be stable despite these energies growing transiently. Here a broadly applicable method to verify global stability of such flows is presented. It uses polynomial optimization computations to construct nonquadratic Lyapunov functions that decrease monotonically. The method is used to verify global stability of 2D plane Couette flow at Reynolds numbers above the the energy stability threshold found by Orr in 1907 [The stability or instability of the steady motions of a perfect liquid and of a viscous liquid. Part II: A viscous liquid, Proc. R. Ir. Acad. Sect. A 27, 69 (1907)]. This is the first global stability result for any flow that surpasses the energy method.

Revista



Revista ISSN
Physical Review Letters 0031-9007

Métricas Externas



PlumX Altmetric Dimensions

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Disciplinas de Investigación



WOS
Physics, Multidisciplinary
Scopus
Sin Disciplinas
SciELO
Sin Disciplinas

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Publicaciones WoS (Ediciones: ISSHP, ISTP, AHCI, SSCI, SCI), Scopus, SciELO Chile.

Colaboración Institucional



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Autores - Afiliación



Ord. Autor Género Institución - País
1 Fuentes, Federico Hombre Cornell University - Estados Unidos
Pontificia Universidad Católica de Chile - Chile
CORNELL UNIV - Estados Unidos
2 Goluskin, David Hombre University of Victoria - Canadá
Univ Victoria - Canadá
3 Chernyshenko, Sergei Hombre Imperial College London - Reino Unido
Imperial Coll London - Reino Unido

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Financiamiento



Fuente
National Science Foundation
Natural Sciences and Engineering Research Council of Canada
National Science Foundation (NSF)
Engineering and Physical Sciences Research Council
NSERC
UK Engineering and Physical Sciences Research Council

Muestra la fuente de financiamiento declarada en la publicación.

Agradecimientos



Agradecimiento
We thank the Geophysical Fluid Dynamics program at Woods Hole Oceanographic Institution, which hosted two of us (F. F. and D. G.) during much of this work. Many helpful discussions with Giovanni Fantuzzi are appreciated, and one of us (F. F.) thanks A. Townsend for computer resources provided at Cornell University. During this work, F. F. was supported by the National Science Foundation (NSF) Grant No. 2012658, D. G. was supported by the NSERC Discovery Grants Program through Grants No. RGPIN-2018-04263, No. RGPAS-2018-522657, and No. DGECR-2018-00371, and S. C. was supported by the UK Engineering and Physical Sciences Research Council Grant No. EP/J011126/1.
We thank the Geophysical Fluid Dynamics program at Woods Hole Oceanographic Institution, which hosted two of us (F. F. and D. G.) during much of this work. Many helpful discussions with Giovanni Fantuzzi are appreciated, and one of us (F. F.) thanks A. Townsend for computer resources provided at Cornell University. During this work, F. F. was supported by the National Science Foundation (NSF) Grant No. 2012658, D. G. was supported by the NSERC Discovery Grants Program through Grants No. RGPIN-2018-04263, No. RGPAS-2018-522657, and No. DGECR-2018-00371, and S. C. was supported by the UK Engineering and Physical Sciences Research Council Grant No. EP/J011126/1.

Muestra la fuente de financiamiento declarada en la publicación.