Moored observations of mesoscale features in the Cape Basin: characteristics and local impacts on water mass distributions

• Published in: Ocean science 2018-09, Vol.14 (5), p.923-945
• Main Authors: Kersale, Marion, Lamont, Tarron, Speich, Sabrina, Terre, Thierry, Laxenaire, Remi, Roberts, Mike J, van den Berg, Marcel A, Ansorge, Isabelle J
• Format: Article
• Language: English
• Subjects: Advection; Analysis; Anomalies; Atlantic Meridional Overturning Circulation (AMOC); Continental slope; Current meter moorings; Current rings; Data; Datasets; Deep sea moorings; Dynamics; Echo sounding; Echoes; Eddies; Exchanging; Filaments; Mass; Mass distribution; Mesoscale eddies; Mesoscale features; Mesoscale phenomena; Methods; Mooring; Observations; Ocean circulation; Oceans; Recording; Satellite altimetry; Satellites; Sciences of the Universe; Submarine banks; Thermohaline circulation; Upwelling; Upwelling (Oceanography); Vortices; Water column; Water depth; Water mass distribution; Water mass intrusions; Water masses
• ISSN: 1812-0792; 1812-0784; 1812-0792
• DOI: 10.5194/os-14-923-2018

The eastern side of the South Atlantic Meridional overturning circulation Basin-wide Array (SAMBA) along 34.5° S is used to assess the nonlinear, mesoscale dynamics of the Cape Basin. This array presently consists of current meter moorings and bottom mounted Current and Pressure recording Inverted Echo Sounders (CPIES) deployed across the continental slope. These data, available from September 2014 to December 2015, combined with satellite altimetry allow us to investigate the characteristics and the impact of mesoscale dynamics on local water mass distribution and cross-validate the different data sets. We demonstrate that the moorings are affected by the complex dynamics of the Cape Basin involving Agulhas rings, cyclonic eddies and anticyclonic eddies from the Agulhas Bank and the South Benguela upwelling front and filaments. Our analyses show that exchange of water masses happens through the advection of water by mesoscale eddies but also via wide water mass intrusions engendered by the existence of intense dipoles. These complex dynamics induce strong intra-seasonal upper-ocean velocity variations and water mass exchanges between the shelf and the open ocean but also across the subantarctic and subtropical waters. This work presents the first independent observations comparison between full-depth moorings and CPIES data sets within the eastern South Atlantic region that gives some evidence of eastern boundary buoyancy anomalies associated with migrating eddies. It also highlights the need to continuously sample the full water depth as inter-basin exchanges occur intermittently and affect the whole water column.