Iodine 129/CFC 11 transit times for Denmark Strait Overflow Water in the Labrador and Irminger Seas

Iodine 129 discharged from nuclear fuel reprocessing plants in France and the United Kingdom is transported into the Nordic Seas on timescales of 3 - 5 years. Tracer I-129 is subsequently injected into intermediate waters that overflow the sills between Greenland, Iceland, and Scotland and ventilate...

Full description

Bibliographic Details
Published in:Journal of Geophysical Research
Main Authors: Smith, Jn, Jones, Ep, Moran, Sb, Smethie, Wm, Kieser, We
Format: Text
Language:English
Published: Amer Geophysical Union 2005
Subjects:
envir
hist
Greenland
Irminger Sea
Denmark Strait
Iceland
Labrador Sea
NADW
Nordic Seas
North Atlantic
Online Access:https://doi.org/10.1029/2004JC002516
https://archimer.ifremer.fr/doc/00232/34344/32757.pdf
https://archimer.ifremer.fr/doc/00232/34344/
Description
Summary:Iodine 129 discharged from nuclear fuel reprocessing plants in France and the United Kingdom is transported into the Nordic Seas on timescales of 3 - 5 years. Tracer I-129 is subsequently injected into intermediate waters that overflow the sills between Greenland, Iceland, and Scotland and ventilate the North Atlantic Deep Waters ( NADW). During the early 1990s, discharges of I-129 increased by 600%, resulting in a large, well- resolved tracer " front'' whose passage through the Nordic Seas is presently being observed by a time series of I-129 measurements on the WOCE ( AR7W) section in the Labrador Sea. The highest I-129 levels were measured below depths of 3000 m in Denmark Strait Overflow Water ( DSOW). These levels increased by about 300% between 1997 and 2001 to values > 40 x 10(7) atoms/ L, indicating that the leading edge of the tracer " front'' from the early 1990s was being observed entering the NADW. Using a simple mixing/ advection model, I-129 and CFC 11 results were used to calculate transit times of 0.4 - 2.6 years for the flow of DSOW from formation regions in the Nordic Seas to the Labrador Sea. Measurements on samples collected in the Irminger Sea in 2001 gave transit times of 0.3 years for core DSOW immediately south of Denmark Strait and about 2 years for locations off the southern tip of Greenland. An increase in DSOW transit times observed in the Labrador Sea between 1999 and 2001 probably reflects a more general weakening in the subpolar gyre of the North Atlantic during the 1990s.

Similar Items