Please use this identifier to cite or link to this item: http://dspace.mediu.edu.my:8181/xmlui/handle/10261/5269
Full metadata record
DC FieldValueLanguage
dc.creatorPrego, R.-
dc.creatorBarciela, Mª del Carmen-
dc.creatorPark, Y. H.-
dc.creatorMorvan, J.-
dc.creatorPoncin, J.-
dc.creatorTréguer, P.-
dc.date2008-06-24T12:19:01Z-
dc.date2008-06-24T12:19:01Z-
dc.date1999-
dc.date.accessioned2017-01-31T01:46:58Z-
dc.date.available2017-01-31T01:46:58Z-
dc.identifierScientia Marina 63(2): 121-127 (1999)-
dc.identifier0214-8358-
dc.identifierhttp://hdl.handle.net/10261/5269-
dc.identifier1886-8134-
dc.identifier.urihttp://dspace.mediu.edu.my:8181/xmlui/handle/10261/5269-
dc.descriptionPublicación online disponible en: http://www.icm.csic.es/scimar/index.php-
dc.descriptionThe subantarctic frontal zone surveyed during the April-May 1991 SUZIL cruise in the Crozet-Kerguelen-Amsterdam area shows a strong horizontal (north to south) gradient of dissolved silicate, increasing with depth, from 5 to 10 µmolSi kg-1 at 100 m, and 10 to 70 µmolSi kg-1 at 600 m. The northern limit of this frontal zone, which is formed by the confluence of the Subtropical and Subantarctic Fronts, is delimited at the surface by the 2 µmolSi kg-1 silicate isoline. Silicate-salinity diagrams also allow different water regimes to be positioned relative to the frontal zone. This sloping interface is between two water bodies, one to the north with more saline subtropical waters of less concentrated silicate than the southern one, corresponding to subantarctic waters which are less saline and richer in silicate. It is concluded that dissolved silicate can be used as a useful tracer of frontal zone water masses in the Indian sector of the Southern Ocean, providing a sound complement to other hydrographic data.-
dc.descriptionThis paper is supported by the Spanish project, ANT90-123-E, financed by the Comisión Interministerial de Ciencia y Tecnología.-
dc.descriptionPeer reviewed-
dc.format449355 bytes-
dc.formatapplication/pdf-
dc.languageeng-
dc.publisherCSIC - Instituto de Ciencias del Mar (ICM)-
dc.rightsopenAccess-
dc.subjectSilicate-
dc.subjectTracer-
dc.subjectFrontal zone-
dc.subjectSilicate-salinity diagram-
dc.subjectCrozet Basin-
dc.subjectSouthern Ocean-
dc.titleOn the distribution of silicic acid as a frontal zone tracer in the Indian sector of the Southern Ocean-
dc.typeArtículo-
Appears in Collections:Digital Csic

Files in This Item:
There are no files associated with this item.


Items in DSpace are protected by copyright, with all rights reserved, unless otherwise indicated.