Dense bottom layers in the Scotia Sea, Southern Ocean: Creation, lifespan, and destruction

Meredith, Michael P. ORCID:; Brown, Peter J.; Naveira Garabato, Alberto C.; Jullion, Loïc; Venables, Hugh J.; Messias, Marie-José. 2013 Dense bottom layers in the Scotia Sea, Southern Ocean: Creation, lifespan, and destruction. Geophysical Research Letters, 40 (5). 933-936.

Before downloading, please read NORA policies.
grl50260.pdf - Published Version

Download (793kB) | Preview


The lower limb of the Atlantic overturning circulation is renewed by dense waters from the Southern Ocean, a substantial portion of which flow through the Scotia Sea. We report dense bottom layers here, with gradients in temperature and salinity comparable to those seen near the surface of the Southern Ocean. These are overlain by layers with much weaker stratification, and are caused by episodic overflows of dense waters across the South Scotia Ridge, and topographic trapping within deep trenches. One such layer was found to be at least 3–4 years older than the water immediately above. The estimated vertical diffusivity to which this layer was subject is substantially less than the strong basin-average deep mixing reported previously. We conjecture that (a) vertical mixing in the Scotia Sea is strongly spatially inhomogeneous, and (b) the flushing of these layers, like their formation, is related to overflow events, and hence also strongly episodic.

Item Type: Publication - Article
Digital Object Identifier (DOI):
Programmes: BAS Programmes > Polar Science for Planet Earth (2009 - ) > Polar Oceans
ISSN: 00948276
Additional Information. Not used in RCUK Gateway to Research.: Not subject to U.S. copyright. Published 2013 American Geophysical Union. Further reproduction or electronic distribution is not permitted.
Date made live: 25 Apr 2013 08:34 +0 (UTC)

Actions (login required)

View Item View Item

Document Downloads

Downloads for past 30 days

Downloads per month over past year

More statistics for this item...