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...

Ausführliche Beschreibung

Gespeichert in:
Bibliographische Detailangaben
Veröffentlicht in:Journal of fluid mechanics 2012-10, Vol.708, p.5-44
Hauptverfasser: Mashayek, A., Peltier, W. R.
Format: Artikel
Sprache:eng
Schlagworte:
Online-Zugang:Volltext
Tags: Tag hinzufügen
Keine Tags, Fügen Sie den ersten Tag hinzu!
container_end_page 44
container_issue
container_start_page 5
container_title Journal of fluid mechanics
container_volume 708
creator Mashayek, A.
Peltier, W. R.
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.
doi_str_mv 10.1017/jfm.2012.304
format Article
fullrecord <record><control><sourceid>proquest_cross</sourceid><recordid>TN_cdi_proquest_miscellaneous_1709752765</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><cupid>10_1017_jfm_2012_304</cupid><sourcerecordid>2767545881</sourcerecordid><originalsourceid>FETCH-LOGICAL-c464t-904bb62a80795ad155d21181c6ae9876ac13897a7baff85fb00501bd7f8f542b3</originalsourceid><addsrcrecordid>eNqNkd9qFDEUhwdRcK3e-QABEbzYGXMy-TNzKaVqoVCh9Xo4ySTbLLPJmswq9aqPoT5en8SsXUSLF14Fcr58h_x-VfUcaAMU1Ou12zSMAmtayh9UC-Cyr5Xk4mG1oJSxGoDRx9WTnNeUQkt7tah-XF5Zcnvz7WuMtzffSXQkWxPDiOma-JBn1H7ys7eZbJM1u5RjGcyR5Dnh7J23I8lXFhNxU_xCymXIBY-hIR8wzQTIxa8pTn4VClvUn63ZA0uyRZ98WC0JhpHohH78e-PT6pHDKdtnh_Oo-vj25PL4fX12_u70-M1Zbbjkc91TrrVk2FHVCxxBiJEBdGAk2r5TEg20Xa9QaXSuE05TKijoUbnOCc50e1S9uvNuU_y0s3keNj4bO00YbNzlAVRJSjAlxf-gwDvRcyjoi3voOu5SKB8ZgHLRyl5CV6jlHWVSzDlZN2yT35TwCzTsOx1Kp8O-06F0WvCXBylmg5MrcRuff79hspVM0rZwzUGLG538uLJ_bv-H-Cf2M7O7</addsrcrecordid><sourcetype>Aggregation Database</sourcetype><iscdi>true</iscdi><recordtype>article</recordtype><pqid>1045369618</pqid></control><display><type>article</type><title>The ‘zoo’ of secondary instabilities precursory to stratified shear flow transition. 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>$$Uhttp://pascal-francis.inist.fr/vibad/index.php?action=getRecordDetail&amp;idt=26362603$$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. R.</creator><general>Cambridge University Press</general><scope>IQODW</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>3V.</scope><scope>7TB</scope><scope>7U5</scope><scope>7UA</scope><scope>7XB</scope><scope>88I</scope><scope>8FD</scope><scope>8FE</scope><scope>8FG</scope><scope>8FK</scope><scope>8G5</scope><scope>ABJCF</scope><scope>ABUWG</scope><scope>AFKRA</scope><scope>ARAPS</scope><scope>AZQEC</scope><scope>BENPR</scope><scope>BGLVJ</scope><scope>BHPHI</scope><scope>BKSAR</scope><scope>C1K</scope><scope>CCPQU</scope><scope>DWQXO</scope><scope>F1W</scope><scope>FR3</scope><scope>GNUQQ</scope><scope>GUQSH</scope><scope>H8D</scope><scope>H96</scope><scope>HCIFZ</scope><scope>KR7</scope><scope>L.G</scope><scope>L6V</scope><scope>L7M</scope><scope>M2O</scope><scope>M2P</scope><scope>M7S</scope><scope>MBDVC</scope><scope>P5Z</scope><scope>P62</scope><scope>PCBAR</scope><scope>PQEST</scope><scope>PQQKQ</scope><scope>PQUKI</scope><scope>PTHSS</scope><scope>Q9U</scope><scope>S0W</scope></search><sort><creationdate>20121010</creationdate><title>The ‘zoo’ of secondary instabilities precursory to stratified shear flow transition. 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. Techniques, methods, instrumentation and models</topic><topic>Hydrodynamic stability</topic><topic>Instability</topic><topic>Instability of shear flows</topic><topic>Physics</topic><topic>Reynolds number</topic><topic>Secondary instability</topic><topic>Shear</topic><topic>Stability</topic><topic>Stability analysis</topic><topic>Stagnation point</topic><topic>Transition to turbulence</topic><topic>Turbulence</topic><topic>Turbulent flows, convection, and heat transfer</topic><topic>Wavenumber</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Mashayek, A.</creatorcontrib><creatorcontrib>Peltier, W. R.</creatorcontrib><collection>Pascal-Francis</collection><collection>CrossRef</collection><collection>ProQuest Central (Corporate)</collection><collection>Mechanical &amp; Transportation Engineering Abstracts</collection><collection>Solid State and Superconductivity Abstracts</collection><collection>Water Resources Abstracts</collection><collection>ProQuest Central (purchase pre-March 2016)</collection><collection>Science Database (Alumni Edition)</collection><collection>Technology Research Database</collection><collection>ProQuest SciTech Collection</collection><collection>ProQuest Technology Collection</collection><collection>ProQuest Central (Alumni) (purchase pre-March 2016)</collection><collection>Research Library (Alumni Edition)</collection><collection>Materials Science &amp; Engineering Collection</collection><collection>ProQuest Central (Alumni Edition)</collection><collection>ProQuest Central UK/Ireland</collection><collection>Advanced Technologies &amp; Aerospace Collection</collection><collection>ProQuest Central Essentials</collection><collection>ProQuest Central</collection><collection>Technology Collection</collection><collection>Natural Science Collection</collection><collection>Earth, Atmospheric &amp; Aquatic Science Collection</collection><collection>Environmental Sciences and Pollution Management</collection><collection>ProQuest One Community College</collection><collection>ProQuest Central Korea</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Engineering Research Database</collection><collection>ProQuest Central Student</collection><collection>Research Library Prep</collection><collection>Aerospace Database</collection><collection>Aquatic Science &amp; Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy &amp; Non-Living Resources</collection><collection>SciTech Premium Collection</collection><collection>Civil Engineering Abstracts</collection><collection>Aquatic Science &amp; Fisheries Abstracts (ASFA) Professional</collection><collection>ProQuest Engineering Collection</collection><collection>Advanced Technologies Database with Aerospace</collection><collection>Research Library</collection><collection>Science Database</collection><collection>Engineering Database</collection><collection>Research Library (Corporate)</collection><collection>Advanced Technologies &amp; Aerospace Database</collection><collection>ProQuest Advanced Technologies &amp; Aerospace Collection</collection><collection>Earth, Atmospheric &amp; Aquatic Science Database</collection><collection>ProQuest One Academic Eastern Edition (DO NOT USE)</collection><collection>ProQuest One Academic</collection><collection>ProQuest One Academic UKI Edition</collection><collection>Engineering Collection</collection><collection>ProQuest Central Basic</collection><collection>DELNET Engineering &amp; Technology Collection</collection><jtitle>Journal of fluid mechanics</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Mashayek, A.</au><au>Peltier, W. 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>
fulltext fulltext
identifier ISSN: 0022-1120
ispartof Journal of fluid mechanics, 2012-10, Vol.708, p.5-44
issn 0022-1120
1469-7645
language eng
recordid cdi_proquest_miscellaneous_1709752765
source Cambridge University Press Journals Complete
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
url https://sfx.bib-bvb.de/sfx_tum?ctx_ver=Z39.88-2004&ctx_enc=info:ofi/enc:UTF-8&ctx_tim=2024-12-04T14%3A41%3A31IST&url_ver=Z39.88-2004&url_ctx_fmt=infofi/fmt:kev:mtx:ctx&rfr_id=info:sid/primo.exlibrisgroup.com:primo3-Article-proquest_cross&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.genre=article&rft.atitle=The%20%E2%80%98zoo%E2%80%99%20of%20secondary%20instabilities%20precursory%20to%20stratified%20shear%20flow%20transition.%20Part%201%20Shear%20aligned%20convection,%20pairing,%20and%20braid%20instabilities&rft.jtitle=Journal%20of%20fluid%20mechanics&rft.au=Mashayek,%20A.&rft.date=2012-10-10&rft.volume=708&rft.spage=5&rft.epage=44&rft.pages=5-44&rft.issn=0022-1120&rft.eissn=1469-7645&rft.coden=JFLSA7&rft_id=info:doi/10.1017/jfm.2012.304&rft_dat=%3Cproquest_cross%3E2767545881%3C/proquest_cross%3E%3Curl%3E%3C/url%3E&disable_directlink=true&sfx.directlink=off&sfx.report_link=0&rft_id=info:oai/&rft_pqid=1045369618&rft_id=info:pmid/&rft_cupid=10_1017_jfm_2012_304&rfr_iscdi=true