Physics
Scientific paper
May 1999
adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1999georl..26.1325r&link_type=abstract
Geophysical Research Letters, Volume 26, Issue 9, p. 1325-1328
Physics
16
Oceanography: General: Arctic And Antarctic Oceanography, Oceanography: General: Water Masses, Oceanography: Physical: Hydrography
Scientific paper
Denmark Strait is the most important exit for water masses formed in the Arctic Mediterranean Sea and supplies a substantial fraction of the North Atlantic Deep Water. Observations obtained from RV Aranda in August-September 1997 indicate that the water crossing the 620m deep sill is mainly drawn from the intermediate waters of the East Greenland Current. The overflow plume was stratified and capped by a less saline layer as it descended beyond 2000m. The presence of a low salinity lid implies that entrainment of ambient water is small and that the downstream evolution of the plume characteristics is due to mixing, within the plume, between the initial overflow waters. Low salinity, but dense, water from the East Greenland Current flowing over the shelf may cross the shelf break south of the sill and add a less dense fraction to the overflow.
Eriksson Patrick
Grönvall Hannu
Hietala Riikka
Launiainen Jouko
Rudels Bert
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