Freshwater fluxes in the Weddell Gyre: Results from ?18O

Full-depth measurements of ?18O from 2008 to 2010 enclosing the Weddell Gyre in the Southern Ocean are used to investigate the regional freshwater budget. Using complementary salinity, nutrients and oxygen data, a four-component mass balance was applied to quantify the relative contributions of mete...

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Main Authors: Brown, Peter J., Meredith, Michael, Jullion, Loic, Naveira Garabato, Alberto, Torres-Valdes, Sinhue, Holland, Paul, Leng, Melanie J., Venables, Hugh
Format: Article in Journal/Newspaper
Language:English
Published: 2014
Subjects:
Online Access:https://eprints.soton.ac.uk/356911/
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spelling ftsouthampton:oai:eprints.soton.ac.uk:356911 2023-08-27T04:05:35+02:00 Freshwater fluxes in the Weddell Gyre: Results from ?18O Brown, Peter J. Meredith, Michael Jullion, Loic Naveira Garabato, Alberto Torres-Valdes, Sinhue Holland, Paul Leng, Melanie J. Venables, Hugh 2014-01-02 https://eprints.soton.ac.uk/356911/ English eng Brown, Peter J., Meredith, Michael, Jullion, Loic, Naveira Garabato, Alberto, Torres-Valdes, Sinhue, Holland, Paul, Leng, Melanie J. and Venables, Hugh (2014) Freshwater fluxes in the Weddell Gyre: Results from ?18O. Philosophical Transactions of the Royal Society A: Mathematical, Physical and Engineering Sciences, 372 (2019), 20130298. (doi:10.1098/rsta.2013.0298 <http://dx.doi.org/10.1098/rsta.2013.0298>). Article PeerReviewed 2014 ftsouthampton 2023-08-03T22:20:21Z Full-depth measurements of ?18O from 2008 to 2010 enclosing the Weddell Gyre in the Southern Ocean are used to investigate the regional freshwater budget. Using complementary salinity, nutrients and oxygen data, a four-component mass balance was applied to quantify the relative contributions of meteoric water (precipitation/glacial input), sea-ice melt and saline (oceanic) sources. Combination of freshwater fractions with velocity fields derived from a box inverse analysis enabled the estimation of gyre-scale budgets of both freshwater types, with deep water exports found to dominate the budget. Surface net sea-ice melt and meteoric contributions reach 1.8% and 3.2%, respectively, influenced by the summer sampling period, and ?1.7% and +1.7% at depth, indicative of a dominance of sea-ice production over melt and a sizable contribution of shelf waters to deep water mass formation. A net meteoric water export of approximately 37?mSv is determined, commensurate with local estimates of ice sheet outflow and precipitation, and the Weddell Gyre is estimated to be a region of net sea-ice production. These results constitute the first synoptic benchmarking of sea-ice and meteoric exports from the Weddell Gyre, against which future change associated with an accelerating hydrological cycle, ocean climate change and evolving Antarctic glacial mass balance can be determined. Article in Journal/Newspaper Antarc* Antarctic Ice Sheet Sea ice Southern Ocean University of Southampton: e-Prints Soton Antarctic Southern Ocean Weddell
institution Open Polar
collection University of Southampton: e-Prints Soton
op_collection_id ftsouthampton
language English
description Full-depth measurements of ?18O from 2008 to 2010 enclosing the Weddell Gyre in the Southern Ocean are used to investigate the regional freshwater budget. Using complementary salinity, nutrients and oxygen data, a four-component mass balance was applied to quantify the relative contributions of meteoric water (precipitation/glacial input), sea-ice melt and saline (oceanic) sources. Combination of freshwater fractions with velocity fields derived from a box inverse analysis enabled the estimation of gyre-scale budgets of both freshwater types, with deep water exports found to dominate the budget. Surface net sea-ice melt and meteoric contributions reach 1.8% and 3.2%, respectively, influenced by the summer sampling period, and ?1.7% and +1.7% at depth, indicative of a dominance of sea-ice production over melt and a sizable contribution of shelf waters to deep water mass formation. A net meteoric water export of approximately 37?mSv is determined, commensurate with local estimates of ice sheet outflow and precipitation, and the Weddell Gyre is estimated to be a region of net sea-ice production. These results constitute the first synoptic benchmarking of sea-ice and meteoric exports from the Weddell Gyre, against which future change associated with an accelerating hydrological cycle, ocean climate change and evolving Antarctic glacial mass balance can be determined.
format Article in Journal/Newspaper
author Brown, Peter J.
Meredith, Michael
Jullion, Loic
Naveira Garabato, Alberto
Torres-Valdes, Sinhue
Holland, Paul
Leng, Melanie J.
Venables, Hugh
spellingShingle Brown, Peter J.
Meredith, Michael
Jullion, Loic
Naveira Garabato, Alberto
Torres-Valdes, Sinhue
Holland, Paul
Leng, Melanie J.
Venables, Hugh
Freshwater fluxes in the Weddell Gyre: Results from ?18O
author_facet Brown, Peter J.
Meredith, Michael
Jullion, Loic
Naveira Garabato, Alberto
Torres-Valdes, Sinhue
Holland, Paul
Leng, Melanie J.
Venables, Hugh
author_sort Brown, Peter J.
title Freshwater fluxes in the Weddell Gyre: Results from ?18O
title_short Freshwater fluxes in the Weddell Gyre: Results from ?18O
title_full Freshwater fluxes in the Weddell Gyre: Results from ?18O
title_fullStr Freshwater fluxes in the Weddell Gyre: Results from ?18O
title_full_unstemmed Freshwater fluxes in the Weddell Gyre: Results from ?18O
title_sort freshwater fluxes in the weddell gyre: results from ?18o
publishDate 2014
url https://eprints.soton.ac.uk/356911/
geographic Antarctic
Southern Ocean
Weddell
geographic_facet Antarctic
Southern Ocean
Weddell
genre Antarc*
Antarctic
Ice Sheet
Sea ice
Southern Ocean
genre_facet Antarc*
Antarctic
Ice Sheet
Sea ice
Southern Ocean
op_relation Brown, Peter J., Meredith, Michael, Jullion, Loic, Naveira Garabato, Alberto, Torres-Valdes, Sinhue, Holland, Paul, Leng, Melanie J. and Venables, Hugh (2014) Freshwater fluxes in the Weddell Gyre: Results from ?18O. Philosophical Transactions of the Royal Society A: Mathematical, Physical and Engineering Sciences, 372 (2019), 20130298. (doi:10.1098/rsta.2013.0298 <http://dx.doi.org/10.1098/rsta.2013.0298>).
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