The ‘zoo’ of secondary instabilities precursory to stratified shear flow transition. Part 1 Shear aligned convection, pairing, and braid instabilities
We study the competition between various secondary instabilities that co-exist in a preturbulent stratified parallel flow subject to Kelvin–Helmholtz instability. In particular, we investigate whether a secondary braid instability might emerge prior to the overturning of the statically unstable regi...
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description | We study the competition between various secondary instabilities that co-exist in a preturbulent stratified parallel flow subject to Kelvin–Helmholtz instability. In particular, we investigate whether a secondary braid instability might emerge prior to the overturning of the statically unstable regions that develop in the cores of the primary Kelvin–Helmholtz billows. We identify two groups of instabilities on the braid. One group is a shear instability which extracts its energy from the background shear and is suppressed by the straining contribution of the background flow. The other group, which seems to have no precedent in the literature, includes phase-locked modes which grow at the stagnation point on the braid and are almost entirely driven by the straining contributions of the background flow. For the latter group, the braid shear has a negative influence on the growth rate. Our analysis demonstrates that the probability of finite-amplitude growth of both braid instabilities is enhanced with increasing Reynolds number and Richardson number. We also show that the possibility of emergence of braid instabilities decreases with the Prandtl number for the shear modes and increases for the stagnation point instabilities. Through detailed non-separable linear stability analysis, we show that both braid instabilities are fundamentally three dimensional with the shear modes being of small wavenumbers and the stagnation point modes dominating at large wavenumber. |
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Part 1 Shear aligned convection, pairing, and braid instabilities</title><source>Cambridge University Press Journals Complete</source><creator>Mashayek, A. ; Peltier, W. R.</creator><creatorcontrib>Mashayek, A. ; Peltier, W. R.</creatorcontrib><description>We study the competition between various secondary instabilities that co-exist in a preturbulent stratified parallel flow subject to Kelvin–Helmholtz instability. In particular, we investigate whether a secondary braid instability might emerge prior to the overturning of the statically unstable regions that develop in the cores of the primary Kelvin–Helmholtz billows. We identify two groups of instabilities on the braid. One group is a shear instability which extracts its energy from the background shear and is suppressed by the straining contribution of the background flow. The other group, which seems to have no precedent in the literature, includes phase-locked modes which grow at the stagnation point on the braid and are almost entirely driven by the straining contributions of the background flow. For the latter group, the braid shear has a negative influence on the growth rate. Our analysis demonstrates that the probability of finite-amplitude growth of both braid instabilities is enhanced with increasing Reynolds number and Richardson number. We also show that the possibility of emergence of braid instabilities decreases with the Prandtl number for the shear modes and increases for the stagnation point instabilities. Through detailed non-separable linear stability analysis, we show that both braid instabilities are fundamentally three dimensional with the shear modes being of small wavenumbers and the stagnation point modes dominating at large wavenumber.</description><identifier>ISSN: 0022-1120</identifier><identifier>EISSN: 1469-7645</identifier><identifier>DOI: 10.1017/jfm.2012.304</identifier><identifier>CODEN: JFLSA7</identifier><language>eng</language><publisher>Cambridge, UK: Cambridge University Press</publisher><subject>Braiding ; Earth, ocean, space ; Exact sciences and technology ; External geophysics ; Fluid dynamics ; Fluid flow ; Fluid mechanics ; Fundamental areas of phenomenology (including applications) ; Geophysics. Techniques, methods, instrumentation and models ; Hydrodynamic stability ; Instability ; Instability of shear flows ; Physics ; Reynolds number ; Secondary instability ; Shear ; Stability ; Stability analysis ; Stagnation point ; Transition to turbulence ; Turbulence ; Turbulent flows, convection, and heat transfer ; Wavenumber</subject><ispartof>Journal of fluid mechanics, 2012-10, Vol.708, p.5-44</ispartof><rights>Copyright © Cambridge University Press 2012</rights><rights>2015 INIST-CNRS</rights><rights>Copyright © Cambridge University Press 2012</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c464t-904bb62a80795ad155d21181c6ae9876ac13897a7baff85fb00501bd7f8f542b3</citedby><cites>FETCH-LOGICAL-c464t-904bb62a80795ad155d21181c6ae9876ac13897a7baff85fb00501bd7f8f542b3</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktohtml>$$Uhttps://www.cambridge.org/core/product/identifier/S0022112012003047/type/journal_article$$EHTML$$P50$$Gcambridge$$H</linktohtml><link.rule.ids>164,315,782,786,27931,27932,55635</link.rule.ids><backlink>$$Uhttp://pascal-francis.inist.fr/vibad/index.php?action=getRecordDetail&idt=26362603$$DView record in Pascal Francis$$Hfree_for_read</backlink></links><search><creatorcontrib>Mashayek, A.</creatorcontrib><creatorcontrib>Peltier, W. R.</creatorcontrib><title>The ‘zoo’ of secondary instabilities precursory to stratified shear flow transition. Part 1 Shear aligned convection, pairing, and braid instabilities</title><title>Journal of fluid mechanics</title><addtitle>J. Fluid Mech</addtitle><description>We study the competition between various secondary instabilities that co-exist in a preturbulent stratified parallel flow subject to Kelvin–Helmholtz instability. In particular, we investigate whether a secondary braid instability might emerge prior to the overturning of the statically unstable regions that develop in the cores of the primary Kelvin–Helmholtz billows. We identify two groups of instabilities on the braid. One group is a shear instability which extracts its energy from the background shear and is suppressed by the straining contribution of the background flow. The other group, which seems to have no precedent in the literature, includes phase-locked modes which grow at the stagnation point on the braid and are almost entirely driven by the straining contributions of the background flow. For the latter group, the braid shear has a negative influence on the growth rate. Our analysis demonstrates that the probability of finite-amplitude growth of both braid instabilities is enhanced with increasing Reynolds number and Richardson number. We also show that the possibility of emergence of braid instabilities decreases with the Prandtl number for the shear modes and increases for the stagnation point instabilities. Through detailed non-separable linear stability analysis, we show that both braid instabilities are fundamentally three dimensional with the shear modes being of small wavenumbers and the stagnation point modes dominating at large wavenumber.</description><subject>Braiding</subject><subject>Earth, ocean, space</subject><subject>Exact sciences and technology</subject><subject>External geophysics</subject><subject>Fluid dynamics</subject><subject>Fluid flow</subject><subject>Fluid mechanics</subject><subject>Fundamental areas of phenomenology (including applications)</subject><subject>Geophysics. Techniques, methods, instrumentation and models</subject><subject>Hydrodynamic stability</subject><subject>Instability</subject><subject>Instability of shear flows</subject><subject>Physics</subject><subject>Reynolds number</subject><subject>Secondary instability</subject><subject>Shear</subject><subject>Stability</subject><subject>Stability analysis</subject><subject>Stagnation point</subject><subject>Transition to turbulence</subject><subject>Turbulence</subject><subject>Turbulent flows, convection, and heat transfer</subject><subject>Wavenumber</subject><issn>0022-1120</issn><issn>1469-7645</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2012</creationdate><recordtype>article</recordtype><sourceid>8G5</sourceid><sourceid>ABUWG</sourceid><sourceid>AFKRA</sourceid><sourceid>AZQEC</sourceid><sourceid>BENPR</sourceid><sourceid>CCPQU</sourceid><sourceid>DWQXO</sourceid><sourceid>GNUQQ</sourceid><sourceid>GUQSH</sourceid><sourceid>M2O</sourceid><recordid>eNqNkd9qFDEUhwdRcK3e-QABEbzYGXMy-TNzKaVqoVCh9Xo4ySTbLLPJmswq9aqPoT5en8SsXUSLF14Fcr58h_x-VfUcaAMU1Ou12zSMAmtayh9UC-Cyr5Xk4mG1oJSxGoDRx9WTnNeUQkt7tah-XF5Zcnvz7WuMtzffSXQkWxPDiOma-JBn1H7ys7eZbJM1u5RjGcyR5Dnh7J23I8lXFhNxU_xCymXIBY-hIR8wzQTIxa8pTn4VClvUn63ZA0uyRZ98WC0JhpHohH78e-PT6pHDKdtnh_Oo-vj25PL4fX12_u70-M1Zbbjkc91TrrVk2FHVCxxBiJEBdGAk2r5TEg20Xa9QaXSuE05TKijoUbnOCc50e1S9uvNuU_y0s3keNj4bO00YbNzlAVRJSjAlxf-gwDvRcyjoi3voOu5SKB8ZgHLRyl5CV6jlHWVSzDlZN2yT35TwCzTsOx1Kp8O-06F0WvCXBylmg5MrcRuff79hspVM0rZwzUGLG538uLJ_bv-H-Cf2M7O7</recordid><startdate>20121010</startdate><enddate>20121010</enddate><creator>Mashayek, A.</creator><creator>Peltier, W. 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Part 1 Shear aligned convection, pairing, and braid instabilities</title><author>Mashayek, A. ; Peltier, W. R.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c464t-904bb62a80795ad155d21181c6ae9876ac13897a7baff85fb00501bd7f8f542b3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2012</creationdate><topic>Braiding</topic><topic>Earth, ocean, space</topic><topic>Exact sciences and technology</topic><topic>External geophysics</topic><topic>Fluid dynamics</topic><topic>Fluid flow</topic><topic>Fluid mechanics</topic><topic>Fundamental areas of phenomenology (including applications)</topic><topic>Geophysics. 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R.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>The ‘zoo’ of secondary instabilities precursory to stratified shear flow transition. Part 1 Shear aligned convection, pairing, and braid instabilities</atitle><jtitle>Journal of fluid mechanics</jtitle><addtitle>J. Fluid Mech</addtitle><date>2012-10-10</date><risdate>2012</risdate><volume>708</volume><spage>5</spage><epage>44</epage><pages>5-44</pages><issn>0022-1120</issn><eissn>1469-7645</eissn><coden>JFLSA7</coden><abstract>We study the competition between various secondary instabilities that co-exist in a preturbulent stratified parallel flow subject to Kelvin–Helmholtz instability. In particular, we investigate whether a secondary braid instability might emerge prior to the overturning of the statically unstable regions that develop in the cores of the primary Kelvin–Helmholtz billows. We identify two groups of instabilities on the braid. One group is a shear instability which extracts its energy from the background shear and is suppressed by the straining contribution of the background flow. The other group, which seems to have no precedent in the literature, includes phase-locked modes which grow at the stagnation point on the braid and are almost entirely driven by the straining contributions of the background flow. For the latter group, the braid shear has a negative influence on the growth rate. Our analysis demonstrates that the probability of finite-amplitude growth of both braid instabilities is enhanced with increasing Reynolds number and Richardson number. We also show that the possibility of emergence of braid instabilities decreases with the Prandtl number for the shear modes and increases for the stagnation point instabilities. Through detailed non-separable linear stability analysis, we show that both braid instabilities are fundamentally three dimensional with the shear modes being of small wavenumbers and the stagnation point modes dominating at large wavenumber.</abstract><cop>Cambridge, UK</cop><pub>Cambridge University Press</pub><doi>10.1017/jfm.2012.304</doi><tpages>40</tpages></addata></record> |
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subjects | Braiding Earth, ocean, space Exact sciences and technology External geophysics Fluid dynamics Fluid flow Fluid mechanics Fundamental areas of phenomenology (including applications) Geophysics. Techniques, methods, instrumentation and models Hydrodynamic stability Instability Instability of shear flows Physics Reynolds number Secondary instability Shear Stability Stability analysis Stagnation point Transition to turbulence Turbulence Turbulent flows, convection, and heat transfer Wavenumber |
title | The ‘zoo’ of secondary instabilities precursory to stratified shear flow transition. Part 1 Shear aligned convection, pairing, and braid instabilities |
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