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Wind forced variability of the Antarctic circumpolar current south of Africa between 1993 and 2010

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dc.contributor.author Domingues, R
dc.contributor.author Goni, G
dc.contributor.author Swart, S
dc.contributor.author Dong, S
dc.date.accessioned 2015-10-22T10:28:29Z
dc.date.available 2015-10-22T10:28:29Z
dc.date.issued 2014-02
dc.identifier.citation Domingues, R, Goni, G, Swart, S and Dong, S. 2014. Wind forced variability of the Antarctic Circumpolar Current south of Africa between 1993 and 2010. Journal of Geophysical Research: Oceans, Vol. 119(2), pp. 1123-1145 en_US
dc.identifier.issn 2169-9275
dc.identifier.uri http://www.aoml.noaa.gov/phod/domingues_JGR_2014.pdf
dc.identifier.uri http://onlinelibrary.wiley.com/doi/10.1002/2013JC008908/abstract
dc.identifier.uri http://hdl.handle.net/10204/8198
dc.description Copyright: 2014 American Geophysical Union,Washington, USA. Due to copyright restrictions, the attached PDF file only contains the abstract of the full text item. For access to the full text item, please consult the publisher's website. The definitive version of the work is Journal of Geophysical Research: Oceans, Vol. 119(2), pp. 1123-1145 en_US
dc.description.abstract The variability of the Antarctic Circumpolar Current (ACC) system is largely linked to the atmospheric forcing. The objective of this work is to assess the link between local wind forcing mechanisms and the variability of the upper-ocean temperature and the dynamics of the different fronts in the ACC region south of South Africa. To accomplish this, in situ and satellite-derived observations are used between 1993 and 2010. The main finding of this work is that meridional changes in the westerlies linked with the Southern Annular Mode (SAM) drive temperature anomalies in the Ekman layer and changes in the Subantarctic Front (SAF) and Antarctic Polar Front (APF) transports through Ekman dynamics. The development of easterly anomalies between 35°S and 45°S during positive SAM is linked to reduced (increased) SAF (APF) transports and a warmer mixed layer in the ACC. The link between the changes in the wind stress and the SAF and APF transport variations occurs through the development of Ekman pumping anomalies near the frontal boundaries, driving an opposite response on the SAF and APF transports. The observed wind-driven changes in the frontal transports suggest small changes to the net ACC transport. In addition, observations indicate that the SAF and APF locations in this region are not linked to the local wind forcing, emphasizing the importance of other factors (e.g., baroclinic instabilities generated by bottom topography) to changes in the frontal location. Results obtained here highlight the importance of repeat XBT temperature sections and their combined analysis with other in situ and remote sensing observations. en_US
dc.language.iso en en_US
dc.publisher American Geophysical Union en_US
dc.relation.ispartofseries Workflow;14903
dc.subject Southern Ocean en_US
dc.subject Subantarctic front en_US
dc.subject Antarctic Polar front en_US
dc.subject Southern Annular Mode en_US
dc.subject Ekman dynamics en_US
dc.title Wind forced variability of the Antarctic circumpolar current south of Africa between 1993 and 2010 en_US
dc.type Article en_US
dc.identifier.apacitation Domingues, R., Goni, G., Swart, S., & Dong, S. (2014). Wind forced variability of the Antarctic circumpolar current south of Africa between 1993 and 2010. http://hdl.handle.net/10204/8198 en_ZA
dc.identifier.chicagocitation Domingues, R, G Goni, S Swart, and S Dong "Wind forced variability of the Antarctic circumpolar current south of Africa between 1993 and 2010." (2014) http://hdl.handle.net/10204/8198 en_ZA
dc.identifier.vancouvercitation Domingues R, Goni G, Swart S, Dong S. Wind forced variability of the Antarctic circumpolar current south of Africa between 1993 and 2010. 2014; http://hdl.handle.net/10204/8198. en_ZA
dc.identifier.ris TY - Article AU - Domingues, R AU - Goni, G AU - Swart, S AU - Dong, S AB - The variability of the Antarctic Circumpolar Current (ACC) system is largely linked to the atmospheric forcing. The objective of this work is to assess the link between local wind forcing mechanisms and the variability of the upper-ocean temperature and the dynamics of the different fronts in the ACC region south of South Africa. To accomplish this, in situ and satellite-derived observations are used between 1993 and 2010. The main finding of this work is that meridional changes in the westerlies linked with the Southern Annular Mode (SAM) drive temperature anomalies in the Ekman layer and changes in the Subantarctic Front (SAF) and Antarctic Polar Front (APF) transports through Ekman dynamics. The development of easterly anomalies between 35°S and 45°S during positive SAM is linked to reduced (increased) SAF (APF) transports and a warmer mixed layer in the ACC. The link between the changes in the wind stress and the SAF and APF transport variations occurs through the development of Ekman pumping anomalies near the frontal boundaries, driving an opposite response on the SAF and APF transports. The observed wind-driven changes in the frontal transports suggest small changes to the net ACC transport. In addition, observations indicate that the SAF and APF locations in this region are not linked to the local wind forcing, emphasizing the importance of other factors (e.g., baroclinic instabilities generated by bottom topography) to changes in the frontal location. Results obtained here highlight the importance of repeat XBT temperature sections and their combined analysis with other in situ and remote sensing observations. DA - 2014-02 DB - ResearchSpace DP - CSIR KW - Southern Ocean KW - Subantarctic front KW - Antarctic Polar front KW - Southern Annular Mode KW - Ekman dynamics LK - https://researchspace.csir.co.za PY - 2014 SM - 2169-9275 T1 - Wind forced variability of the Antarctic circumpolar current south of Africa between 1993 and 2010 TI - Wind forced variability of the Antarctic circumpolar current south of Africa between 1993 and 2010 UR - http://hdl.handle.net/10204/8198 ER - en_ZA


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