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Tracing water masses with I-129 in the western Nordic Seas in early spring 2002
Responsible organisation
2004 (English)In: Geophysical Research Letters, ISSN 0094-8276, E-ISSN 1944-8007, Vol. 31, no 19Article in journal (Refereed) Published
Abstract [en]

The distribution of I-129 was utilized for labeling water masses in three sections of the western Nordic Seas. An increase of the tracer in Polar Waters of the East Greenland Current was observed between the Fram Strait and 72degreesN section and attributed to either unaccounted Polar Waters and/or recirculation of cold and fresh Atlantic Waters from the West Spitzbergen Current. Recent convection homogenized I-129 in upper 1000 m of the Greenland Sea, and similar concentrations were observed in dense waters of the Denmark Strait. The densest outflow waters were not found in either the Greenland Sea or the East Greenland Current at 72degreesN.

Place, publisher, year, edition, pages
2004. Vol. 31, no 19
National Category
Natural Sciences
Research subject
SWEDARCTIC 2002, Arctic Ocean 2002
Identifiers
URN: urn:nbn:se:polar:diva-3223DOI: 10.1029/2004GL020863OAI: oai:DiVA.org:polar-3223DiVA: diva2:1050214
Available from: 2016-11-28 Created: 2016-11-21 Last updated: 2016-11-28

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CiteExportLink to record
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