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Transition of a Hyperpycnal Flow Into a Saline Turbidity Current Due to Differential Diffusivities

dc.contributor.authorZhao, Liang
dc.contributor.authorOuillon, Raphael
dc.contributor.authorVowinckel, Bernhard
dc.contributor.authorMeiburg, Eckart
dc.contributor.authorKneller, Benjamin
dc.contributor.authorHe, Zhiguo
dc.date.accessioned2019-05-12T23:03:30Z
dc.date.available2019-05-12T23:03:30Z
dc.date.issued2018-11-16
dc.identifier.citationZhao , L , Ouillon , R , Vowinckel , B , Meiburg , E , Kneller , B & He , Z 2018 , ' Transition of a Hyperpycnal Flow Into a Saline Turbidity Current Due to Differential Diffusivities ' , Geophysical Research Letters , vol. 45 , no. 21 , pp. 11,875-11,884 . https://doi.org/10.1029/2018GL080150en
dc.identifier.issn0094-8276
dc.identifier.otherPURE: 140589913
dc.identifier.otherPURE UUID: 6f4cade5-b3e2-4b68-8d8c-86c05f83976f
dc.identifier.otherScopus: 85056430338
dc.identifier.otherScopus: 85056430338
dc.identifier.urihttp://hdl.handle.net/2164/12255
dc.descriptionAcknowledgments: E.M. gratefully acknowledges support through NSF grant CBET‐1438052. L.Z. thanks The National Natural Science Foundation of China (11672267) and the China Scholarship Council for providing him with a scholarship to study at UCSB. B.V. was supported by a Feodor‐Lynen scholarship from the Alexander von Humboldt Foundation, Germany. Computational resources for this work were made available by the Extreme Science and Engineering Discovery Environment (XSEDE), which is supported by NSF grant TGCTS150053. All of the data employed in this work can be obtained at https://drive.google.com/drive/folders/1pfg-sBgZeXcu3GbbrOa62FX87qcozzyl?usp=sharing.en
dc.format.extent10
dc.language.isoeng
dc.relation.ispartofGeophysical Research Lettersen
dc.rights© 2018. American Geophysical Unionen
dc.subjectturbidity currenten
dc.subjecthypercynal flowen
dc.subjectdiffusivityen
dc.subjectQE Geologyen
dc.subjectGeophysicsen
dc.subjectEarth and Planetary Sciences(all)en
dc.subject.lccQEen
dc.titleTransition of a Hyperpycnal Flow Into a Saline Turbidity Current Due to Differential Diffusivitiesen
dc.typeJournal articleen
dc.contributor.institutionUniversity of Aberdeen.Geology and Geophysicsen
dc.description.statusPeer revieweden
dc.description.versionPublisher PDFen
dc.identifier.doihttps://doi.org/10.1029/2018GL080150
dc.date.embargoedUntil2019-05-13
dc.identifier.urlhttp://www.scopus.com/inward/record.url?scp=85056430338&partnerID=8YFLogxKen
dc.identifier.vol45en
dc.identifier.iss21en


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