Isochoric unsteady multipolar spherical oscillations in compressible radial and cylindrical background flows

The multipolar spherical vortex solutions to the Euler and Navier–Stokes equations in background cylindrical flow with swirl admit an additional background divergent radial flow with arbitrary time-dependent amplitude. In this case the radial wavenumber $k$ , fundamental frequency $\omega$ and overall amplitude $U$ of the multipolar mode superposition become time-dependent and related functions. Assumption of an additional constraint, as a constitutive equation defining the time evolution of the spatially homogeneous divergence of the background flow, is required for the time evolution of the total flow to be completely evaluated from the initial conditions. It is found that flow compression implies an increase of the absolute values of the fundamental frequency $\omega$ and overall velocity amplitude $U$ of the oscillations.

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Publication Details

Journal
Journal of Fluid Mechanics
Published
2024-12-26
DOI
https://doi.org/10.1017/jfm.2024.1167
Citations
3
Primary Topic
Geophysics and Gravity Measurements
Type
article
Field-Weighted Citation Impact
1.44

Funders

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article

Isochoric unsteady multipolar spherical oscillations in compressible radial and cylindrical background flows

Álvaro Viúdez
3 citations
Journal of Fluid Mechanics
Geophysics and Gravity Measurements
1.44
article

Isochoric unsteady multipolar spherical oscillations in compressible radial and cylindrical background flows

Álvaro Viúdez
article en
3 citations

Abstract

The multipolar spherical vortex solutions to the Euler and Navier–Stokes equations in background cylindrical flow with swirl admit an additional background divergent radial flow with arbitrary time-dependent amplitude. In this case the radial wavenumber $k$ , fundamental frequency $\omega$ and overall amplitude $U$ of the multipolar mode superposition become time-dependent and related functions. Assumption of an additional constraint, as a constitutive equation defining the time evolution of the spatially homogeneous divergence of the background flow, is required for the time evolution of the total flow to be completely evaluated from the initial conditions. It is found that flow compression implies an increase of the absolute values of the fundamental frequency $\omega$ and overall velocity amplitude $U$ of the oscillations.

Journal of Fluid MechanicsVol. 1002
Institut de Ciències del Mar (ES), Marine Technology Unit (ES)
Ministerio de Ciencia, Innovación y Universidades, Ministerio de Ciencia y Tecnología
Openalex Percentile: Top 18%
Geophysics and Gravity Measurements
1.44
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