Change search
ReferencesLink to record
Permanent link

Direct link
Arctic Ocean freshwater composition, pathways and transformations from a passive tracer simulation
SMHI, Research Department, Oceanography.ORCID iD: 0000-0003-3107-5200
SMHI, Core Services.
SMHI, Research Department, Oceanography.ORCID iD: 0000-0003-1068-746X
2014 (English)In: Tellus. Series A, Dynamic meteorology and oceanography, ISSN 0280-6495, E-ISSN 1600-0870, Vol. 66Article in journal (Refereed) Published
Abstract [en]

Freshwater (FW) induced transformations in the upper Arctic Ocean were studied using a coupled regional sea ice-ocean model driven by winds and thermodynamic forcing from a reanalysis of data during the period 1948-2011, focusing on the mean state during 1968-2011. Using passive tracers to mark a number of FW sources and sinks, their mean composition, pathways and export were examined. The distribution of the simulated FW height reproduced the known features of the Arctic Ocean and volume-integrated FW content matched climatological estimates reasonably well. Input from Eurasian rivers and extraction by sea-ice formation dominate the composition of the Arctic FW content whilst Pacific water increases in importance in the Canadian Basin. Though pathways generally agreed with previous studies the locus of the Eurasian runoff shelf-basin transport centred at the Alpha-Mendeleyev ridge, shifting the Pacific-Atlantic front eastwards. A strong coupling between tracers representing Eurasian runoff and sea-ice formation showed how water modified on the shelf spreads across the Arctic and mainly exits through the Fram Strait. Transformation to salinity dependent coordinates showed how Atlantic water is modified by both low-salinity shelf and Pacific waters in an estuary-like overturning producing water masses of intermediate salinity that are exported to the Nordic Seas. A total halocline renewal rate of 1.0 Sv, including both shelf-basin exchange and cross-isohaline flux, was estimated from the transports: both components were of equal magnitude. The model's halocline shelf-basin exchange is dominated by runoff and sea-ice processes at the western shelves (the Barents and Kara seas) and Pacific water at the eastern shelves (the Laptev, East Siberian and Chukchi seas).

Place, publisher, year, edition, pages
2014. Vol. 66
Keyword [en]
Arctic Ocean, freshwater, pathways, water mass transformation, passive tracers
National Category
Oceanography, Hydrology, Water Resources
Research subject
Oceanography
Identifiers
URN: urn:nbn:se:smhi:diva-147DOI: 10.3402/tellusa.v66.23988ISI: 000341106800001OAI: oai:DiVA.org:smhi-147DiVA: diva2:801007
Available from: 2015-04-08 Created: 2015-03-26 Last updated: 2016-11-22Bibliographically approved

Open Access in DiVA

fulltext(4904 kB)2 downloads
File information
File name FULLTEXT01.pdfFile size 4904 kBChecksum SHA-512
6a62a6c474ef2286a51a765b46d413b72d2a18f94388d06233e5df60b3dd7f79a153d82e7e26d2f14fdcfdaa5ba0d0716931c434bb60425948ec1ef6e7d6a273
Type fulltextMimetype application/pdf

Other links

Publisher's full text

Search in DiVA

By author/editor
Pemberton, PerNilsson, JohanMeier, Markus
By organisation
OceanographyCore Services
In the same journal
Tellus. Series A, Dynamic meteorology and oceanography
Oceanography, Hydrology, Water Resources

Search outside of DiVA

GoogleGoogle Scholar
Total: 2 downloads
The number of downloads is the sum of all downloads of full texts. It may include eg previous versions that are now no longer available

Altmetric score

Total: 19 hits
ReferencesLink to record
Permanent link

Direct link