The diffusive regime of double-diffusive convection

The diffusive regime of double-diffusive convection is discussed, with a particular focus on unresolved issues that are holding up the development of large-scale parameterizations. Some of these issues, such as interfacial transports and layer-interface interactions, may be studied in isolation. Lab...

Ausführliche Beschreibung

Gespeichert in:
Bibliographische Detailangaben
Veröffentlicht in:Progress in oceanography 2003-03, Vol.56 (3-4), p.461-481
Hauptverfasser: Kelley, D.E., Fernando, H.J.S., Gargett, A.E., Tanny, J., Özsoy, E.
Format: Artikel
Sprache:eng
Online-Zugang:Volltext
Tags: Tag hinzufügen
Keine Tags, Fügen Sie den ersten Tag hinzu!
container_end_page 481
container_issue 3-4
container_start_page 461
container_title Progress in oceanography
container_volume 56
creator Kelley, D.E.
Fernando, H.J.S.
Gargett, A.E.
Tanny, J.
Özsoy, E.
description The diffusive regime of double-diffusive convection is discussed, with a particular focus on unresolved issues that are holding up the development of large-scale parameterizations. Some of these issues, such as interfacial transports and layer-interface interactions, may be studied in isolation. Laboratory work should help with these. However, we must also face more difficult matters that relate to oceanic phenomena that are not represented easily in the laboratory. These lie beneath some fundamental questions about how double-diffusive structures are formed in the ocean, and how they evolve in the competitive ocean environment.
doi_str_mv 10.1016/S0079-6611(03)00026-0
format Article
fullrecord <record><control><sourceid>proquest_cross</sourceid><recordid>TN_cdi_proquest_miscellaneous_18026537</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><sourcerecordid>18026537</sourcerecordid><originalsourceid>FETCH-LOGICAL-c381t-6b9806baf97199fa4290f43da8a931c8e38c3306495e08e47adb9ec83322a0e63</originalsourceid><addsrcrecordid>eNpFkE9LxDAQxXNQcF39CEJPoofqpNOmyVEW_8GCB9dzSNOJVtpmTdoFv73trujpDe89Bt6PsQsONxy4uH0FKFUqBOdXgNcAkIkUjtjizz5hpzF-zgGIbMFw80FJ3Tg3xmZHSaD3pqPEu6T2Y9VS-h9Z3-_IDo3vz9ixM22k819dsreH-83qKV2_PD6v7tapRcmHVFRKgqiMUyVXypk8U-ByrI00CrmVhNIigshVQSApL01dKbISMcsMkMAluzz83Qb_NVIcdNdES21revJj1FxO6wosp2JxKNrgYwzk9DY0nQnfmoOeseg9Fj3v14B6j2U6fgC2k1bZ</addsrcrecordid><sourcetype>Aggregation Database</sourcetype><iscdi>true</iscdi><recordtype>article</recordtype><pqid>18026537</pqid></control><display><type>article</type><title>The diffusive regime of double-diffusive convection</title><source>Elsevier ScienceDirect Journals Complete - AutoHoldings</source><creator>Kelley, D.E. ; Fernando, H.J.S. ; Gargett, A.E. ; Tanny, J. ; Özsoy, E.</creator><creatorcontrib>Kelley, D.E. ; Fernando, H.J.S. ; Gargett, A.E. ; Tanny, J. ; Özsoy, E.</creatorcontrib><description>The diffusive regime of double-diffusive convection is discussed, with a particular focus on unresolved issues that are holding up the development of large-scale parameterizations. Some of these issues, such as interfacial transports and layer-interface interactions, may be studied in isolation. Laboratory work should help with these. However, we must also face more difficult matters that relate to oceanic phenomena that are not represented easily in the laboratory. These lie beneath some fundamental questions about how double-diffusive structures are formed in the ocean, and how they evolve in the competitive ocean environment.</description><identifier>ISSN: 0079-6611</identifier><identifier>DOI: 10.1016/S0079-6611(03)00026-0</identifier><language>eng</language><ispartof>Progress in oceanography, 2003-03, Vol.56 (3-4), p.461-481</ispartof><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c381t-6b9806baf97199fa4290f43da8a931c8e38c3306495e08e47adb9ec83322a0e63</citedby><cites>FETCH-LOGICAL-c381t-6b9806baf97199fa4290f43da8a931c8e38c3306495e08e47adb9ec83322a0e63</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><link.rule.ids>314,780,784,27923,27924</link.rule.ids></links><search><creatorcontrib>Kelley, D.E.</creatorcontrib><creatorcontrib>Fernando, H.J.S.</creatorcontrib><creatorcontrib>Gargett, A.E.</creatorcontrib><creatorcontrib>Tanny, J.</creatorcontrib><creatorcontrib>Özsoy, E.</creatorcontrib><title>The diffusive regime of double-diffusive convection</title><title>Progress in oceanography</title><description>The diffusive regime of double-diffusive convection is discussed, with a particular focus on unresolved issues that are holding up the development of large-scale parameterizations. Some of these issues, such as interfacial transports and layer-interface interactions, may be studied in isolation. Laboratory work should help with these. However, we must also face more difficult matters that relate to oceanic phenomena that are not represented easily in the laboratory. These lie beneath some fundamental questions about how double-diffusive structures are formed in the ocean, and how they evolve in the competitive ocean environment.</description><issn>0079-6611</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2003</creationdate><recordtype>article</recordtype><recordid>eNpFkE9LxDAQxXNQcF39CEJPoofqpNOmyVEW_8GCB9dzSNOJVtpmTdoFv73trujpDe89Bt6PsQsONxy4uH0FKFUqBOdXgNcAkIkUjtjizz5hpzF-zgGIbMFw80FJ3Tg3xmZHSaD3pqPEu6T2Y9VS-h9Z3-_IDo3vz9ixM22k819dsreH-83qKV2_PD6v7tapRcmHVFRKgqiMUyVXypk8U-ByrI00CrmVhNIigshVQSApL01dKbISMcsMkMAluzz83Qb_NVIcdNdES21revJj1FxO6wosp2JxKNrgYwzk9DY0nQnfmoOeseg9Fj3v14B6j2U6fgC2k1bZ</recordid><startdate>20030301</startdate><enddate>20030301</enddate><creator>Kelley, D.E.</creator><creator>Fernando, H.J.S.</creator><creator>Gargett, A.E.</creator><creator>Tanny, J.</creator><creator>Özsoy, E.</creator><scope>AAYXX</scope><scope>CITATION</scope><scope>7TG</scope><scope>7TN</scope><scope>F1W</scope><scope>H96</scope><scope>KL.</scope><scope>L.G</scope></search><sort><creationdate>20030301</creationdate><title>The diffusive regime of double-diffusive convection</title><author>Kelley, D.E. ; Fernando, H.J.S. ; Gargett, A.E. ; Tanny, J. ; Özsoy, E.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c381t-6b9806baf97199fa4290f43da8a931c8e38c3306495e08e47adb9ec83322a0e63</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2003</creationdate><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Kelley, D.E.</creatorcontrib><creatorcontrib>Fernando, H.J.S.</creatorcontrib><creatorcontrib>Gargett, A.E.</creatorcontrib><creatorcontrib>Tanny, J.</creatorcontrib><creatorcontrib>Özsoy, E.</creatorcontrib><collection>CrossRef</collection><collection>Meteorological &amp; Geoastrophysical Abstracts</collection><collection>Oceanic Abstracts</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Aquatic Science &amp; Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy &amp; Non-Living Resources</collection><collection>Meteorological &amp; Geoastrophysical Abstracts - Academic</collection><collection>Aquatic Science &amp; Fisheries Abstracts (ASFA) Professional</collection><jtitle>Progress in oceanography</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Kelley, D.E.</au><au>Fernando, H.J.S.</au><au>Gargett, A.E.</au><au>Tanny, J.</au><au>Özsoy, E.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>The diffusive regime of double-diffusive convection</atitle><jtitle>Progress in oceanography</jtitle><date>2003-03-01</date><risdate>2003</risdate><volume>56</volume><issue>3-4</issue><spage>461</spage><epage>481</epage><pages>461-481</pages><issn>0079-6611</issn><abstract>The diffusive regime of double-diffusive convection is discussed, with a particular focus on unresolved issues that are holding up the development of large-scale parameterizations. Some of these issues, such as interfacial transports and layer-interface interactions, may be studied in isolation. Laboratory work should help with these. However, we must also face more difficult matters that relate to oceanic phenomena that are not represented easily in the laboratory. These lie beneath some fundamental questions about how double-diffusive structures are formed in the ocean, and how they evolve in the competitive ocean environment.</abstract><doi>10.1016/S0079-6611(03)00026-0</doi><tpages>21</tpages><oa>free_for_read</oa></addata></record>
fulltext fulltext
identifier ISSN: 0079-6611
ispartof Progress in oceanography, 2003-03, Vol.56 (3-4), p.461-481
issn 0079-6611
language eng
recordid cdi_proquest_miscellaneous_18026537
source Elsevier ScienceDirect Journals Complete - AutoHoldings
title The diffusive regime of double-diffusive convection
url https://sfx.bib-bvb.de/sfx_tum?ctx_ver=Z39.88-2004&ctx_enc=info:ofi/enc:UTF-8&ctx_tim=2025-01-08T09%3A10%3A13IST&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%20diffusive%20regime%20of%20double-diffusive%20convection&rft.jtitle=Progress%20in%20oceanography&rft.au=Kelley,%20D.E.&rft.date=2003-03-01&rft.volume=56&rft.issue=3-4&rft.spage=461&rft.epage=481&rft.pages=461-481&rft.issn=0079-6611&rft_id=info:doi/10.1016/S0079-6611(03)00026-0&rft_dat=%3Cproquest_cross%3E18026537%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=18026537&rft_id=info:pmid/&rfr_iscdi=true