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dc.contributor.authorMenezes, Viviane V.  Concept link
dc.contributor.authorMacdonald, Alison M.  Concept link
dc.contributor.authorSchatzman, Courtney  Concept link
dc.date.accessioned2017-02-14T20:29:21Z
dc.date.available2017-02-14T20:29:21Z
dc.date.issued2017-01-25
dc.identifier.citationScience Advances 3 (2017): e1601426en_US
dc.identifier.urihttp://hdl.handle.net/1912/8717
dc.description© The Author(s), 2017. This article is distributed under the terms of the Creative Commons Attribution License. The definitive version was published in Science Advances 3 (2017): e1601426, doi:10.1126/sciadv.1601426.en_US
dc.description.abstractSouthern Ocean abyssal waters, in contact with the atmosphere at their formation sites around Antarctica, not only bring signals of a changing climate with them as they move around the globe but also contribute to that change through heat uptake and sea level rise. A repeat hydrographic line in the Indian sector of the Southern Ocean, occupied three times in the last two decades (1994, 2007, and, most recently, 2016), reveals that Antarctic Bottom Water (AABW) continues to become fresher (0.004 ± 0.001 kg/g decade−1), warmer (0.06° ± 0.01°C decade−1), and less dense (0.011 ± 0.002 kg/m3 decade−1). The most recent observations in the Australian-Antarctic Basin show a particularly striking acceleration in AABW freshening between 2007 and 2016 (0.008 ± 0.001 kg/g decade−1) compared to the 0.002 ± 0.001 kg/g decade−1 seen between 1994 and 2007. Freshening is, in part, responsible for an overall shift of the mean temperature-salinity curve toward lower densities. The marked freshening may be linked to an abrupt iceberg-glacier collision and calving event that occurred in 2010 on the George V/Adélie Land Coast, the main source region of bottom waters for the Australian-Antarctic Basin. Because AABW is a key component of the global overturning circulation, the persistent decrease in bottom water density and the associated increase in steric height that result from continued warming and freshening have important consequences beyond the Southern Indian Ocean.en_US
dc.description.sponsorshipThe 2016 I08S cruise and the analysis and science performed at sea, as well as the individual principal investigators were funded through multiple National Oceanic and Atmospheric Administration (NOAA) and NSF grants including NSF grant OCE-1437015. The research for this article was mainly completed at sea. For land-based work, V.V.M. relied on her postdoctoral funding through NSF grant OCE-1435665, and A.M.M. was supported in part by NSF grant OCE-1356630 and NOAA grant NA11OAR4310063.en_US
dc.language.isoen_USen_US
dc.publisherAmerican Association for the Advancement of Scienceen_US
dc.relation.urihttps://doi.org/10.1126/sciadv.1601426
dc.rightsAttribution-NonCommercial 4.0 International*
dc.rights.urihttp://creativecommons.org/licenses/by-nc/4.0/*
dc.subjectSalinityen_US
dc.subjectAABWen_US
dc.subjectChangesen_US
dc.subjectWater massesen_US
dc.subjectT-S propertiesen_US
dc.subjectIcebergen_US
dc.subjectCalvingen_US
dc.subjectAntarticaen_US
dc.subjectAbyssen_US
dc.subjectClimate changeen_US
dc.titleAccelerated freshening of Antarctic Bottom Water over the last decade in the Southern Indian Oceanen_US
dc.typeArticleen_US
dc.identifier.doi10.1126/sciadv.1601426


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Attribution-NonCommercial 4.0 International
Except where otherwise noted, this item's license is described as Attribution-NonCommercial 4.0 International