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Letters to Nature
Nature 407, 66-69 (7 September 2000) | doi:10.1038/35024048; Received 2 March 2000; Accepted 22 June 2000
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Mid-depth recirculation observed in the interior Labrador and Irminger seas by direct velocity measurements
Kara L. Lavender1, Russ E. Davis1 & W. Brechner Owens2
- Scripps Institution of Oceanography, University of California, San Diego, La Jolla, California 92093-0230, USA
- Woods Hole Oceanographic Institution , Woods Hole, Massachusetts 02543, USA
Correspondence to: Kara L. Lavender1 Correspondence and requests for materials should be addressed to K.L.L. (e-mail: Email: klavender@ucsd.edu)
Abstract
The Labrador Sea is one of the sites where convection exports surface water
to the deep ocean in winter as part of the thermohaline circulation. Labrador
Sea water is characteristically cold and fresh, and it can be traced at intermediate
depths (500–2,000 m) across the North Atlantic Ocean, to the
south and to the east of the Labrador Sea1, 2, 3. Widespread
observations of the ocean currents that lead to this distribution of Labrador
Sea water have, however, been difficult and therefore scarce. We have used
more than 200 subsurface floats to measure directly basin-wide horizontal
velocities at various depths in the Labrador and Irminger seas. We observe
unanticipated recirculations of the mid-depth (
700 m) cyclonic
boundary currents in both basins, leading to an anticyclonic flow in the interior
of the Labrador basin. About 40% of the floats from the region of deep convection
left the basin within one year and were rapidly transported in the anticyclonic
flow to the Irminger basin, and also eastwards into the subpolar gyre. Surprisingly,
the float tracks did not clearly depict the deep western boundary current,
which is the expected main pathway of Labrador Sea water in the thermohaline
circulation. Rather, the flow along the boundary near Flemish Cap is dominated
by eddies that transport water offshore. Our detailed observations of the
velocity structure with a high data coverage suggest that we may have to revise
our picture of the formation and spreading of Labrador Sea water, and future
studies with similar instrumentation will allow new insights on the intermediate
depth ocean circulation.
- Scripps Institution of Oceanography, University of California, San Diego, La Jolla, California 92093-0230, USA
- Woods Hole Oceanographic Institution , Woods Hole, Massachusetts 02543, USA
Correspondence to: Kara L. Lavender1 Correspondence and requests for materials should be addressed to K.L.L. (e-mail: Email: klavender@ucsd.edu)
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