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Agulhas current meanders facilitate shelf-slope exchange on the Eastern Agulhas Bank

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dc.contributor.author Malan, N
dc.contributor.author Backeberg, Bjorn-Christoph
dc.contributor.author Biastoch, A
dc.contributor.author Durgadoo, JV
dc.contributor.author Samuelsen, A
dc.contributor.author Reason, C
dc.contributor.author Hermes, J
dc.date.accessioned 2018-07-20T09:01:51Z
dc.date.available 2018-07-20T09:01:51Z
dc.date.issued 2018-06
dc.identifier.citation Malan, N. et al. 2018. Agulhas current meanders facilitate shelf-slope exchange on the Eastern Agulhas Bank. Journal of Geophysical Research: Oceans, vol. 123: 10.1029/2017JC013602 en_US
dc.identifier.issn 2169-9291
dc.identifier.issn 2169-9275
dc.identifier.uri https://doi.org/10.1029/2017JC013602
dc.identifier.uri https://agupubs.onlinelibrary.wiley.com/doi/abs/10.1029/2017JC013602
dc.identifier.uri http://hdl.handle.net/10204/10318
dc.description Article published in Journal of Geophysical Research: Oceans, vol. 123: 10.1029/2017JC013602. ©2018. American Geophysical Union. en_US
dc.description.abstract Large solitary meanders are arguably the dominant mode of variability in the Agulhas Current. Observational studies have shown that these large meanders are associated with strong upwelling velocities and affect the shelf circulation for over 100 days per year. Here 10-year time series from two ocean general circulation models are used to create a composite picture of the Agulhas Current and its interactions with the shelf circulation in meandering and nonmeandering modes. Both models show good agreement with the size, propagation speed, and frequency of observed meanders. These composite meanders are then used to examine the response of shelf waters to the onset of large meanders, with the use of model output enabling the dynamics at depth to be explored. Results show a composite mean warming of up to 3 degrees C of depth-averaged temperature along the shelf edge associated with an intrusion of the current jet onto the shelf driven by an intensification of the flow along the leading edge of large meanders. However, this intensification of flow results in cooling of bottom waters, driving cold events at the shelf break of <10 degrees C at 100 m. Thus, the intensification of the current jet associated with large meander events appears to drive strong up and downwelling events across the inshore front of the Agulhas Current, facilitating shelf-slope exchange. en_US
dc.language.iso en en_US
dc.publisher Agulhas current meanders facilitate shelf-slope exchange on the Eastern Agulhas Bank en_US
dc.relation.ispartofseries Worklist;21096
dc.subject Agulhas Current en_US
dc.subject Circulation models en_US
dc.subject Shelf-slope en_US
dc.subject Ocean temperature en_US
dc.title Agulhas current meanders facilitate shelf-slope exchange on the Eastern Agulhas Bank en_US
dc.type Article en_US
dc.identifier.apacitation Malan, N., Backeberg, B., Biastoch, A., Durgadoo, J., Samuelsen, A., Reason, C., & Hermes, J. (2018). Agulhas current meanders facilitate shelf-slope exchange on the Eastern Agulhas Bank. http://hdl.handle.net/10204/10318 en_ZA
dc.identifier.chicagocitation Malan, N, Bjorn-Christoph Backeberg, A Biastoch, JV Durgadoo, A Samuelsen, C Reason, and J Hermes "Agulhas current meanders facilitate shelf-slope exchange on the Eastern Agulhas Bank." (2018) http://hdl.handle.net/10204/10318 en_ZA
dc.identifier.vancouvercitation Malan N, Backeberg B, Biastoch A, Durgadoo J, Samuelsen A, Reason C, et al. Agulhas current meanders facilitate shelf-slope exchange on the Eastern Agulhas Bank. 2018; http://hdl.handle.net/10204/10318. en_ZA
dc.identifier.ris TY - Article AU - Malan, N AU - Backeberg, Bjorn-Christoph AU - Biastoch, A AU - Durgadoo, JV AU - Samuelsen, A AU - Reason, C AU - Hermes, J AB - Large solitary meanders are arguably the dominant mode of variability in the Agulhas Current. Observational studies have shown that these large meanders are associated with strong upwelling velocities and affect the shelf circulation for over 100 days per year. Here 10-year time series from two ocean general circulation models are used to create a composite picture of the Agulhas Current and its interactions with the shelf circulation in meandering and nonmeandering modes. Both models show good agreement with the size, propagation speed, and frequency of observed meanders. These composite meanders are then used to examine the response of shelf waters to the onset of large meanders, with the use of model output enabling the dynamics at depth to be explored. Results show a composite mean warming of up to 3 degrees C of depth-averaged temperature along the shelf edge associated with an intrusion of the current jet onto the shelf driven by an intensification of the flow along the leading edge of large meanders. However, this intensification of flow results in cooling of bottom waters, driving cold events at the shelf break of <10 degrees C at 100 m. Thus, the intensification of the current jet associated with large meander events appears to drive strong up and downwelling events across the inshore front of the Agulhas Current, facilitating shelf-slope exchange. DA - 2018-06 DB - ResearchSpace DP - CSIR KW - Agulhas Current KW - Circulation models KW - Shelf-slope KW - Ocean temperature LK - https://researchspace.csir.co.za PY - 2018 SM - 2169-9291 SM - 2169-9275 T1 - Agulhas current meanders facilitate shelf-slope exchange on the Eastern Agulhas Bank TI - Agulhas current meanders facilitate shelf-slope exchange on the Eastern Agulhas Bank UR - http://hdl.handle.net/10204/10318 ER - en_ZA


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