Please use this identifier to cite or link to this item: http://hdl.handle.net/10397/92778
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dc.contributorDepartment of Aeronautical and Aviation Engineeringen_US
dc.creatorGao, Len_US
dc.creatorGuo, HFen_US
dc.creatorYu, SCMen_US
dc.date.accessioned2022-05-16T09:07:42Z-
dc.date.available2022-05-16T09:07:42Z-
dc.identifier.issn0022-1120en_US
dc.identifier.urihttp://hdl.handle.net/10397/92778-
dc.language.isoenen_US
dc.publisherCambridge University Pressen_US
dc.rightsThis article has been published in a revised form in Journal of Fluid Mechanics https://doi.org/10.1017/jfm.2019.1050. This version is free to view and download for private research and study only. Not for re-distribution or re-use. © The Author(s), 2020.en_US
dc.rightsWhen citing an Accepted Manuscript or an earlier version of an article, the Cambridge University Press requests that readers also cite the Version of Record with a DOI link. The article is subsequently published in revised form in Journal of Fluid Mechanics https://dx.doi.org/10.1017/jfm.2019.1050.en_US
dc.subjectBaroclinic flowsen_US
dc.subjectJetsen_US
dc.subjectVortex dynamicsen_US
dc.titleA general definition of formation time for starting jets and forced plumes at low Richardson numberen_US
dc.typeJournal/Magazine Articleen_US
dc.identifier.volume886en_US
dc.identifier.doi10.1017/jfm.2019.1050en_US
dcterms.abstractAs an important dimensionless parameter for the vortex formation process, the general form of the formation time defined by Dabiri (Annu. Rev. Fluid Mech., vol. 41, 2009, pp. 17-33) is refined so as to provide better normalization for various vortex generator configurations. Our proposed definition utilizes the total circulation over the entire flow domain rather than that of the forming vortex ring alone. It adopts an integral form by considering the instantaneous infinitesimal increment in the formation time so that the effect of temporally varying properties of the flow configuration can be accounted for properly. By including the effect of buoyancy, the specific form of the general formation time for the starting forced plumes with negative and positive buoyancy is derived. A theoretical prediction based on the Kelvin-Benjamin variational principle shows that the general formation time manifests the invariance of the critical time scale, i.e.The formation number, under the influence of a source-Ambient density difference. It demonstrates that the general formation time, based on the circulation production over the entire flow field, could take into account the effect of various vorticity production mechanisms, such as from a flux term or in a baroclinic fluid, on the critical formation number. The proposed definition may, therefore, serve as a guideline for deriving the specific form of the formation time in other types of starting/pulsatile flows.en_US
dcterms.accessRightsopen accessen_US
dcterms.bibliographicCitationJournal of fluid mechanics, 10 Mar. 2020, v. 886, A6en_US
dcterms.isPartOfJournal of fluid mechanicsen_US
dcterms.issued2020-03-
dc.identifier.scopus2-s2.0-85077963215-
dc.identifier.eissn1469-7645en_US
dc.identifier.artnA6en_US
dc.description.validate202205 bckwen_US
dc.description.oaAccepted Manuscripten_US
dc.identifier.FolderNumberAAE-0094-
dc.description.fundingSourceOthersen_US
dc.description.fundingTextNational Natural Science Foundation of China; The Hong Kong Polytechnic Universityen_US
dc.description.pubStatusPublisheden_US
dc.identifier.OPUS42717417-
dc.description.oaCategoryGreen (AAM)en_US
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