A deep hydrological front between intermediate and deep-water masses in the glacial Indian Ocean

A deep hydrological front between intermediate and deep-water masses in the glacial Indian Ocean

Ocean circulation and climate are strongly interconnected. A reconstruction of the hydrological structure of the deep and intermediate water of the Indian Ocean during the last glacial maximum is discussed.

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Bibliographische Detailangaben
Veröffentlicht in:Nature (London) 1988-06, Vol.333 (6174), p.651-655
Hauptverfasser: KALLEL, N, LABEYRIE, L. D, JUILLET-LECLERC, A, DUPLESSY, J.-C
Format: Artikel
Sprache:eng
Schlagworte:
Deep water
Earth sciences
Earth, ocean, space
Exact sciences and technology
Geology
Intermediate water
Isotope geochemistry
Isotope geochemistry. Geochronology
Marine and continental quaternary
Ocean circulation
Oceanography
Surficial geology
Water circulation
Weather
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Beschreibung
Zusammenfassung:Ocean circulation and climate are strongly interconnected. A reconstruction of the hydrological structure of the deep and intermediate water of the Indian Ocean during the last glacial maximum is discussed.
ISSN:0028-0836
1476-4687
DOI:10.1038/333651a0