dc.contributor.author | Midttun, Lars | |
dc.date.accessioned | 2012-07-03T09:12:46Z | |
dc.date.available | 2012-07-03T09:12:46Z | |
dc.date.issued | 1984 | |
dc.identifier.citation | This report is not to be cited without prior reference to the author | no_NO |
dc.identifier.uri | http://hdl.handle.net/11250/103993 | |
dc.description.abstract | Formation of heavy bottom water through rejection of brine
during ide freezing is a regular phenomenon in the Barents Sea,
particular on the Novaya Zemlya shelf, but also observed in
other shallow localities of the sea.
Water with temperature around -1°C and salinity above 34.95
is found moving eastwards on the southern side of the Novaya
Zemlya-Franz Josef Land Channel which communicates with the
Polar Sea. The relative high salinity is a result of admixture
from heavy water formed during the freezing process. | no_NO |
dc.language.iso | eng | no_NO |
dc.publisher | ICES | no_NO |
dc.relation.ispartofseries | ICES CM Documents;1984/C:17 | |
dc.subject | salinity | no_NO |
dc.subject | salinitet | no_NO |
dc.title | Formation of heavy bottom water in the Barents Sea | no_NO |
dc.type | Working paper | no_NO |
dc.subject.nsi | VDP::Mathematics and natural science: 400::Zoology and botany: 480::Marine biology: 497 | no_NO |
dc.subject.nsi | VDP::Mathematics and natural science: 400::Geosciences: 450::Oceanography: 452 | no_NO |
dc.source.pagenumber | 16 s. | no_NO |