Observations of Thermohaline Convection adjacent to Brunt Ice Shelf
Fer, Ilker; Makinson, Keith ORCID: https://orcid.org/0000-0002-5791-1767; Nicholls, Keith W. ORCID: https://orcid.org/0000-0002-2188-4509. 2012 Observations of Thermohaline Convection adjacent to Brunt Ice Shelf. Journal of Physical Oceanography, 42 (3). 502-508. 10.1175/JPO-D-11-0211.1
Before downloading, please read NORA policies.Preview |
Text
Copyright American Meteorological Society. jpo-d-11-0211%2E1.pdf - Published Version Download (1MB) | Preview |
Abstract/Summary
Observations were made of ocean microstructure and horizontal currents adjacent to Brunt Ice Shelf in the southeastern Weddell Sea. Periods of in situ supercooled water extending as deep as 65 m were associated with ice nucleation and frazil formation at depth. Ascending ice crystals due to convection lead to increased dissipation rates. The main outflow of potentially supercooled water from deep beneath ice shelf is suggested to be in the deep channel northeast of the measurement site. Because this water is advected southward along the front, it becomes in situ supercooled, leading to suspended ice formation, thermohaline convection, and enhanced dissipation.
Item Type: | Publication - Article |
---|---|
Digital Object Identifier (DOI): | 10.1175/JPO-D-11-0211.1 |
Programmes: | BAS Programmes > Polar Science for Planet Earth (2009 - ) > Polar Oceans |
ISSN: | 0022-3670 |
Additional Keywords: | Sea-ice, Turbulence, Dissipation, Model, Layer |
Date made live: | 01 May 2012 09:34 +0 (UTC) |
URI: | https://nora.nerc.ac.uk/id/eprint/17919 |
Actions (login required)
View Item |
Document Downloads
Downloads for past 30 days
Downloads per month over past year