2013
DOI: 10.1260/1475-472x.12.7-8.719
|View full text |Cite
|
Sign up to set email alerts
|

On Sound Emission by Acoustic Sources in a Shear Flow

Abstract: The Green's function for the plane unidirectional shear flow is obtained without restriction to either the high or low frequencies, that is in an exact form that applies also to local wavelengths comparable to the lengthscale of variation of the shear velocity of the mean flow. The method is a version of the variation of constants, and applies to any velocity profile for which the free wave solution of the unforced wave equation is available. The hyperbolic tangent shear velocity profile is taken as an example… Show more

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
1
1

Citation Types

0
2
0

Year Published

2016
2016
2018
2018

Publication Types

Select...
2

Relationship

0
2

Authors

Journals

citations
Cited by 2 publications
(2 citation statements)
references
References 73 publications
(178 reference statements)
0
2
0
Order By: Relevance
“…The acoustic-vortical wave equation (61)≡(79b) for the pressure perturbation spectrum of a wave (57) of frequency ω and axial k and azimuthal m wavenumber specifies the radial dependence and involves the frequency with Doppler shift (79a) due to the nonuniform shear U and swirl Ω; the coefficients D , E , and source term Z~ are given by equations (62a,b; 63a,b). The acoustic-vortical wave equation (79b) in the absence of swirl Ω=0 reduces to the acoustic-shear wave equations (61; 62a,b; 63a,b) written most often for plane homentropic flow, 20–23 for which two sets of exact solutions are known: (i) for homentropic mean flow; 2436 (ii) for nonhomentropic isentropic mean flow. 37,38 The wave equation (79b) has a singularity at critical layer where the Doppler shifted frequency (79a) vanishes (80a) …”
Section: Wave Propagation Generation and Energy Balancementioning
confidence: 99%
See 1 more Smart Citation
“…The acoustic-vortical wave equation (61)≡(79b) for the pressure perturbation spectrum of a wave (57) of frequency ω and axial k and azimuthal m wavenumber specifies the radial dependence and involves the frequency with Doppler shift (79a) due to the nonuniform shear U and swirl Ω; the coefficients D , E , and source term Z~ are given by equations (62a,b; 63a,b). The acoustic-vortical wave equation (79b) in the absence of swirl Ω=0 reduces to the acoustic-shear wave equations (61; 62a,b; 63a,b) written most often for plane homentropic flow, 20–23 for which two sets of exact solutions are known: (i) for homentropic mean flow; 2436 (ii) for nonhomentropic isentropic mean flow. 37,38 The wave equation (79b) has a singularity at critical layer where the Doppler shifted frequency (79a) vanishes (80a) …”
Section: Wave Propagation Generation and Energy Balancementioning
confidence: 99%
“…[39][40][41] Thus, a critical layer and a continuous spectrum exists for: (i) acoustic-vortical waves in any shear flow, e.g. plane homentropic with linear, [24][25][26][27][28][29][30][31][32][33][34][35][36][37] exponential, 32 hyperbolic tangent, 33,35 or parabolic 34 velocity profile; (ii) acoustic-vortical waves in any shear flow, e.g. plane homenergetic, that is isentropic but nonhomentropic; 37,38 (iii) acoustic-vortical waves in any swirling flow, with the exception of rigid body swirl.…”
Section: Compressive Shear and Swirl Wave Forcingmentioning
confidence: 99%