The cold-core eddy and strong upwelling off the coast of New South Wales in early 2007

• Published in: Deep-sea research. Part II, Topical studies in oceanography Vol. 58; no. 5; pp. 574 - 591
• Main Authors: Oke, Peter R., Griffin, David A.
• Format: Journal Article
• Language: English
• Published: Elsevier Ltd 01.03.2011
• Subjects: Anomalies; Circulation; Coastal environments; Deep sea; East Australian Current; Eddies; Eddy; Enrichment; Marine; Ocean models; Ocean Reanalysis; Upwelling; Upwelling; Ocean Reanalysis; Eddy; East Australian Current
• ISSN: 0967-0645; 1879-0100
• DOI: 10.1016/j.dsr2.2010.06.006

During the Austral summer of 2006–07 a series of extreme oceanic events occurred in the Tasman Sea. Following a series of strong wind-driven upwelling events, an intense cold-core eddy developed off Sydney, Australia. A data-assimilating, eddy-resolving ocean model is used to create a three-dimensional time-varying reanalysis of these events. The reanalysis indicates that the cold anomalies associated with the upwellings were in excess of −5 °C near the coast, where sea level decreased by as much as 0.2 m. The reanalysed three-dimensional structure of the cold-core eddy shows the eddy "leaning" to the west–north–west, in towards the continental shelf. The diameter of the eddy is about 100 km and the sea-level anomaly at the eddy centre peaks at around −1 m, with an associated sub-surface temperature anomaly in excess of −8 °C at 200 m depth, corresponding to an upward isotherm excursion of 600 m. The circulation around the cyclonic eddy is ageostrophic, with upwelling in the southern sector of the eddy (where flow is onshore and climbing the continental slope) and downwelling in the northern sector (where flow is descending off the slope). Three-dimensional trajectories of water parcels around the eddy involve 50-100-m vertical excursions. Based on the reanalysed circulation and composite satellite images of Chlorophyll-a, we hypothesise that the circulation around the eddy led to significant nutrient enrichment in the euphotic zone around the perimeter of the eddy.