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Project details

Title: Submesoscale processes – billows and eddies – along the productive shelf by the East Australian Current
Id: 2536
Investigator(s): Iain Suthers
University of New South Wales - School of Biological, Earth and Environmental Sciences [details]

Description: scientific objectives: 1.Examine the entrainment shelf water and the amount of eddy uplift driven in relation to the strength of the adjacent EAC, coastal wind, the coastal counter-current, and slope canyons; and to quantify oceanographic behaviour of frontal eddies including their movement; 2.Compare the zooplankton size structure and the bioacoustic biomass between coastal waters, frontal eddies and the adjacent EAC or Tasman Sea; 3.Similarly compare the phytoplankton (prokaryotic and eukaryotic) biomass, diversity of pigments and other molecular markers and biogeochemical functions across coastal, EAC and frontal eddy water masses, 4.Similarly compare the zooplankton size structure and species diversity, the larval fish size distribution and the bioacoustic biomass; 5.The abundance, condition and genetic traits of other zooplankton (lobster phyllosoma).
Years: 2015

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Survey InvestigatorDescription
IN2015_V03

[details]
I. Suthers (UNSW-SIMS) Frontal eddies or "billows" are ubiquitous, small cyclonic eddies <100 km in diameter, and regularly characterise the continental side of all ocean boundary currents. They occur approximately weekly, and last up to 3 weeks which is sufficient for the early life history of fish. The physics and biology of these ubiquitous eddies are not understood. They are not resolved by present-day surface altimetry, but are evident along the East Australian Current (EAC) in SST or in real-time surface currents from the Coffs Harbour HF Radar (30.5°S). We will determine if uplift within the eddy nurtures plankton in comparison to the inner shelf water; and in comparison to similar eddies offshore around the EAC retroflection. We expect entrainment of adjacent shelf water is preconditioned to sustain larval fish, compared to entrainment of Tasman Sea water. We expect the condition and size distribution (survival) of larval fish will be greater in frontal eddies than in source water on the shelf or in the EAC. Frontal eddies may be a general mechanism for recruitment to coastal fisheries, such as for the Kuroshio Current, Gulf Stream, Agulhas Current. We will continue our long-term observations of phytoplankton, salps, krill, larval fish assemblages and eddy behaviour in this important region. We will investigate 2 to 3 frontal eddies on 2 separate occasions in the following possible locations: * the EAC separation zone south of North Stradbroke Island (27.6°S); or * south of Cape Byron (28.6°S); * south of Smoky Cape (30.9°S), * under the Coffs Harbour HF radar (30°S) * south of Seal Rocks/Sugarloaf Point (32.4°S) and off Port Stephens (32.7°S) or Sydney (34°S). Our scientific objectives are to: 1. Examine the entrainment shelf water and the amount of eddy uplift driven in relation to the strength of the adjacent EAC, coastal wind, the coastal counter-current, and slope canyons; and to quantify oceanographic behaviour of frontal eddies including their movement; 2. Compare the zooplankton size structure and the bioacoustic biomass between coastal waters, frontal eddies and the adjacent EAC or Tasman Sea; 3. Similarly compare the phytoplankton (prokaryotic and eukaryotic) biomass, diversity of pigments and other molecular markers and biogeochemical functions across coastal, EAC and frontal eddy water masses, 4. Similarly compare the zooplankton size structure and species diversity, the larval fish size distribution and the bioacoustic biomass; 5. The abundance, condition and genetic traits of other zooplankton (lobster phyllosoma).
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