CO2-Induced Ocean Warming of the Antarctic Continental Shelf in an Eddying Global Climate Model

Persistent Link:
http://hdl.handle.net/10150/626296
Title:
CO2-Induced Ocean Warming of the Antarctic Continental Shelf in an Eddying Global Climate Model
Author:
Goddard, Paul B. ( 0000-0002-4954-8988 ) ; Dufour, Carolina O. ( 0000-0002-1441-3880 ) ; Yin, Jianjun ( 0000-0002-3335-2171 ) ; Griffies, Stephen M. ( 0000-0002-3711-236X ) ; Winton, Michael ( 0000-0001-7982-0260 )
Affiliation:
Univ Arizona, Dept Geosci
Issue Date:
2017-10
Publisher:
AMER GEOPHYSICAL UNION
Citation:
CO2-Induced Ocean Warming of the Antarctic Continental Shelf in an Eddying Global Climate Model 2017, 122 (10):8079 Journal of Geophysical Research: Oceans
Journal:
Journal of Geophysical Research: Oceans
Rights:
© 2017. American Geophysical Union. All Rights Reserved.
Collection Information:
This item from the UA Faculty Publications collection is made available by the University of Arizona with support from the University of Arizona Libraries. If you have questions, please contact us at repository@u.library.arizona.edu.
Abstract:
Ocean warming near the Antarctic ice shelves has critical implications for future ice sheet mass loss and global sea level rise. A global climate model with an eddying ocean is used to quantify the mechanisms contributing to ocean warming on the Antarctic continental shelf in an idealized 2xCO(2) experiment. The results indicate that relatively large warm anomalies occur both in the upper 100 m and at depths above the shelf floor, which are controlled by different mechanisms. The near-surface ocean warming is primarily a response to enhanced onshore advective heat transport across the shelf break. The deep shelf warming is initiated by onshore intrusions of relatively warm Circumpolar Deep Water (CDW), in density classes that access the shelf, as well as the reduction of the vertical mixing of heat. CO2-induced shelf freshening influences both warming mechanisms. The shelf freshening slows vertical mixing by limiting gravitational instabilities and the upward diffusion of heat associated with CDW, resulting in the buildup of heat at depth. Meanwhile, freshening near the shelf break enhances the lateral density gradient of the Antarctic Slope Front (ASF) and disconnect isopycnals between the shelf and CDW, making cross-ASF heat exchange more difficult. However, at several locations along the ASF, the cross-ASF heat transport is less inhibited and heat can move onshore. Once onshore, lateral and vertical heat advection work to disperse the heat anomalies across the shelf region. Understanding the inhomogeneous Antarctic shelf warming will lead to better projections of future ice sheet mass loss.
Note:
Green Open Access: AGU allows final articles to be placed in an institutional repository 6 months after publication. / 6 month embargo; Published online 25 OCT 2017
ISSN:
21699275
DOI:
10.1002/2017JC012849
Keywords:
eddying climate model; Antarctica shelf warming; Antarctica shelf freshening
Version:
Final published version
Sponsors:
National Oceanic and Atmospheric Administration (NOAA) CPO project [NA13OAR4310128]; National Science Foundation [OPP-1513411]; University of Arizona faculty startup funding; University of Arizona Department of Geosciences; National Aeronautics and Space Administration (NASA) [NNX14AL40G]; Princeton Environmental Institute (PEI) Grand Challenge initiative; Southern Ocean Carbon and Climate Observations and Modeling (SOCCOM) project under the National Science Foundation [PLR-1425989]
Additional Links:
http://doi.wiley.com/10.1002/2017JC012849

Full metadata record

DC FieldValue Language
dc.contributor.authorGoddard, Paul B.en
dc.contributor.authorDufour, Carolina O.en
dc.contributor.authorYin, Jianjunen
dc.contributor.authorGriffies, Stephen M.en
dc.contributor.authorWinton, Michaelen
dc.date.accessioned2017-12-21T19:42:48Z-
dc.date.available2017-12-21T19:42:48Z-
dc.date.issued2017-10-
dc.identifier.citationCO2-Induced Ocean Warming of the Antarctic Continental Shelf in an Eddying Global Climate Model 2017, 122 (10):8079 Journal of Geophysical Research: Oceansen
dc.identifier.issn21699275-
dc.identifier.doi10.1002/2017JC012849-
dc.identifier.urihttp://hdl.handle.net/10150/626296-
dc.description.abstractOcean warming near the Antarctic ice shelves has critical implications for future ice sheet mass loss and global sea level rise. A global climate model with an eddying ocean is used to quantify the mechanisms contributing to ocean warming on the Antarctic continental shelf in an idealized 2xCO(2) experiment. The results indicate that relatively large warm anomalies occur both in the upper 100 m and at depths above the shelf floor, which are controlled by different mechanisms. The near-surface ocean warming is primarily a response to enhanced onshore advective heat transport across the shelf break. The deep shelf warming is initiated by onshore intrusions of relatively warm Circumpolar Deep Water (CDW), in density classes that access the shelf, as well as the reduction of the vertical mixing of heat. CO2-induced shelf freshening influences both warming mechanisms. The shelf freshening slows vertical mixing by limiting gravitational instabilities and the upward diffusion of heat associated with CDW, resulting in the buildup of heat at depth. Meanwhile, freshening near the shelf break enhances the lateral density gradient of the Antarctic Slope Front (ASF) and disconnect isopycnals between the shelf and CDW, making cross-ASF heat exchange more difficult. However, at several locations along the ASF, the cross-ASF heat transport is less inhibited and heat can move onshore. Once onshore, lateral and vertical heat advection work to disperse the heat anomalies across the shelf region. Understanding the inhomogeneous Antarctic shelf warming will lead to better projections of future ice sheet mass loss.en
dc.description.sponsorshipNational Oceanic and Atmospheric Administration (NOAA) CPO project [NA13OAR4310128]; National Science Foundation [OPP-1513411]; University of Arizona faculty startup funding; University of Arizona Department of Geosciences; National Aeronautics and Space Administration (NASA) [NNX14AL40G]; Princeton Environmental Institute (PEI) Grand Challenge initiative; Southern Ocean Carbon and Climate Observations and Modeling (SOCCOM) project under the National Science Foundation [PLR-1425989]en
dc.language.isoenen
dc.publisherAMER GEOPHYSICAL UNIONen
dc.relation.urlhttp://doi.wiley.com/10.1002/2017JC012849en
dc.rights© 2017. American Geophysical Union. All Rights Reserved.en
dc.subjecteddying climate modelen
dc.subjectAntarctica shelf warmingen
dc.subjectAntarctica shelf fresheningen
dc.titleCO2-Induced Ocean Warming of the Antarctic Continental Shelf in an Eddying Global Climate Modelen
dc.typeArticleen
dc.contributor.departmentUniv Arizona, Dept Geoscien
dc.identifier.journalJournal of Geophysical Research: Oceansen
dc.description.noteGreen Open Access: AGU allows final articles to be placed in an institutional repository 6 months after publication. / 6 month embargo; Published online 25 OCT 2017en
dc.description.collectioninformationThis item from the UA Faculty Publications collection is made available by the University of Arizona with support from the University of Arizona Libraries. If you have questions, please contact us at repository@u.library.arizona.edu.en
dc.eprint.versionFinal published versionen
dc.contributor.institutionDepartment of Geosciences; University of Arizona; Tucson AZ USA-
dc.contributor.institutionAtmospheric and Oceanic Sciences Program; Princeton University; Princeton NJ USA-
dc.contributor.institutionDepartment of Geosciences; University of Arizona; Tucson AZ USA-
dc.contributor.institutionGeophysical Fluid Dynamics Laboratory; NOAA; Princeton NJ USA-
dc.contributor.institutionGeophysical Fluid Dynamics Laboratory; NOAA; Princeton NJ USA-
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