With the collaboration of: Research supported by:. Water for a Healthy Country. Hypersalinity and phosphorus availability: the role of mineral precipitation in the Coorong. lagoons of South Australia. Milena Fernandes and Jason Tanner. May 2009.
The South Australian Marine Scalefish Fishery. Stock Status Report. Report to PIRSA. AJ Fowler, R McGarvey, MA Steer & JE Feenstra. December 2009. SARDI Publication No. F2007/000565-4. SARDI Research Report Series No. 413. Fowler et al. 2009 MSF
A preliminary consideration of by-catch in the. Marine Scalefish fishery of South Australia. AJ Fowler, M Lloyd, and D Schmarr. May 2009. SARDI Publication Number F2009/000097-1. SARDI Research Report Series Number 365. A preliminary consideration
Inland Waters & Catchment Ecology. Monitoring temporal changes in the species composition and. lateral movement patterns of small-bodied fishes within the inlet and outlet creeks to Banrock Station wetland. SARDI Publication No. F2009/000104-1 SARDI
MMMaaarrriiinnneee EEEnnnvvviiirrrooonnnmmmeeennnttt &&& EEEcccooolllooogggyyy. Pup production assessment of the Australian sea lion Neophoca cinerea at Dangerous Reef. and English Island, South Australia. Photo: R. Harcourt. SARDI Publication
Innovative solutions for aquaculture planning and management: addressing seal interactions in the finfish aquaculture industry SD Goldsworthy, B Page, PD Shaughnessy, D Hamer, KD Peters, RR McIntosh, AMM Baylis, J McKenzie South Australian Research
ASSESSING DIFFERENT SPATIAL SCALES TO ANALYSE SATELLITE TRACKING DATA 175. 9 ASSESSMENT OF DIFFERENT HOME RANGE ESTIMATES AND SPATIAL SCALES TO DESCRIBE THE DISTRIBUTION OF AUSTRALIAN SEA LION FORAGING EFFORT. B Page, KD Peters, RR McIntosh, D Hamer,
Operational interactions of the South Australian. Sardine Fishery with the Common Dolphin:. November 2004 to March 2009. D.J. Hamer, A. Ivey, and T.M. Ward. April 2009. SARDI Aquatic Sciences. Publication No. F2007/001098-2. SARDI Report Series No.
62. 8.3. Summer Circulation and Upwelling. During summer (January to March), strong south-easterly winds over the shelf offshore from the mouth of the gulf create an upwelling favourable environment that results in cooler surface water residing off
79. 9. Conclusions. A 3D primitive equation model was applied to the TFZ to examine the hydrodynamics of the region. Using a nesting process to provide boundary conditions for the TFZ model, the region was represented with high resolution while