The Influence of the Garden Island Causeway on the Environmental Values of the Southern End of Cockburn Sound

The Influence of the Garden Island Causeway on the Environmental Values of the Southern End of Cockburn Sound

p:\csmc\manglesbay\reports\mangles_bay_study.doc 16/09/2002; 3:26 PM THE INFLUENCE OF THE GARDEN ISLAND CAUSEWAY ON THE ENVIRONMENTAL VALUES OF THE SOUTHERN END OF COCKBURN SOUND Prepared for: COCKBURN SOUND MANAGEMENT COUNCIL Prepared by: DAL SCIENCE AND ENGINEERING PTY LTD AUGUST 2002 REPORT NO. 02/247/1 CONTENTS EXECUTIVE SUMMARY __________________________________________________ iv 1. INTRODUCTION________________________________________________________ 9 1.1 GENERAL_________________________________________________________________________9 1.2 BACKGROUND TO THIS STUDY ____________________________________________________10 1.3 STUDY SCOPE AND APPROACH ____________________________________________________10 1.3.1 Scope ________________________________________________________________________10 1.3.2 Approach_____________________________________________________________________11 2. REVIEW OF COCKBURN SOUND CIRCULATION AND MODELLING ______ 14 2.1 CIRCULATION IN COCKBURN SOUND ______________________________________________14 2.2 DETERMINATION OF EXCHANGE (FLUSHING) ______________________________________15 2.3 INFLUENCE OF THE CAUSEWAY ___________________________________________________16 3. CAUSEWAY CIRCULATION MODELLING _______________________________ 18 3.1 APPROACH ______________________________________________________________________18 3.2 MODEL FORCING_________________________________________________________________18 3.3 MODEL GRID_____________________________________________________________________18 3.4 CAUSEWAY CONFIGURATIONS MODELLED ________________________________________19 3.5 THE INFLUENCE OF THE CAUSEWAY ON COCKBURN SOUND ________________________20 3.5.1 The effect of the Causeway on the flushing of Cockburn Sound ___________________________20 3.6 VALIDATION_____________________________________________________________________25 3.6.1 Low Frequency Forcing _________________________________________________________26 3.7 THE INFLUENCE OF THE CAUSEWAY ON THE MANGLES BAY REGION ________________28 3.7.1 Flushing______________________________________________________________________28 3.7.2 Bottom Shear Stress ____________________________________________________________30 4. FIELD SURVEY ________________________________________________________ 32 4.1 INTRODUCTION __________________________________________________________________32 4.2 HYDODYNAMIC INTERPRETATION ________________________________________________32 5. THE EFFECTS OF VARIOUS CAUSEWAY CONFIGURATIONS ON ECOLOGY, COASTAL PROCESSES AND HUMAN USES IN COCKBURN SOUND________________________________________________________________ 37 5.1 ECOLOGY _______________________________________________________________________37 5.1.1 Water quality__________________________________________________________________37 5.1.2 Seagrass _____________________________________________________________________41 5.2 COASTAL PROCESSES ____________________________________________________________49 5.2.1 Effects due to changes in wave energy ______________________________________________49 5.2.2 Longshore sediment transport and shoreline change ___________________________________50 5.3 HUMAN USES ____________________________________________________________________53 5.3.1 Current uses __________________________________________________________________53 5.3.2 Future uses ___________________________________________________________________55 6. CONCLUSIONS AND RECOMMENDATIONS _____________________________ 57 6.1 CONCLUSIONS ___________________________________________________________________57 6.1.1 Flushing and circulation characteristics_____________________________________________57 6.1.2 Ecology ______________________________________________________________________57 6.1.3 Coastal processes ______________________________________________________________58 6.1.4 Human uses ___________________________________________________________________59 6.1.5 Overview _____________________________________________________________________60 6.2 RECOMMENDATIONS _____________________________________________________________61 7. ACKNOWLEDGMENTS ________________________________________________ 62 8. REFERENCES _________________________________________________________ 63 DALSE:CSMC: INFLUENCE ON THE GARDEN ISLAND CAUSEWAY i TABLES Table 2.1 Flushing times for Cockburn Sound ________________________________ 15 Table 3.1 Summary of simulations undertaken using the EFDC model _____________ 20 Table 3.2 The effect of the Causeway on the flushing of Cockburn Sound (summer and autumn) ___________________________________________________ 21 Table 3.3 The effect of the Causeway on the flushing of various areas of Cockburn Sound in summer_______________________________________________ 23 Table 3.4 The effect of the Causeway on the flushing of various areas of Cockburn Sound in autumn _______________________________________________ 24 Table 5.1 Median chlorophyll values in various areas of Cockburn Sound, summer 2001/2002 ____________________________________________________ 39 Table 5.2 Relative impact of various Causeway configurations on summer water quality at the southern end of Cockburn Sound _______________________ 41 Table 5.3 Relative impact of various Causeway configurations on seagrasses. Predictions on shear stress based on peak current velocities during a spring tide in summer ___________________________________________ 48 FIGURES Figure 3.1 Bathymetry (water depth in metres) of the southern region of Cockburn Sound with each of the four Causeway configurations, with model grid overlay _______________________________________________________ 19 Figure 3.2 Changes in dye concentration in Cockburn Sound in summer and autumn, with and without the Causeway_____________________________ 21 Figure 3.3 Areas of Cockburn Sound examined for flushing characteristics __________ 22 Figure 3.4 Changes in dye concentration in various areas of Cockburn Sound in summer, with and without the Causeway ____________________________ 23 Figure 3.5 Changes in dye concentration in various areas of Cockburn Sound in autumn, with and without the Causeway_____________________________ 24 Figure 3.6 Location of current meters used in the validation study _________________ 25 Figure 3.7 Comparison of modelled and field data in the southern entrance of Cockburn Sound _______________________________________________ 27 Figure 3.8 More detailed comparison of modelled and field data in the southern entrance of Cockburn Sound ______________________________________ 27 Figure 3.9 Spectral analysis of modelled and field data for the current meter in the southern entrance of Cockburn Sound_______________________________ 28 Figure 3.10 Initial dye distribution used to investigate the circulation within Mangles Bay. Dye concentration varies between 0 (blue) and 10 (red) ____________ 29 Figure 3.11 Instantaneous dye concentration distribution generated by circulation transporting and mixing the initial dye distribution on the 26th of January 17:30, 1998 ___________________________________________________ 30 DALSE:CSMC: INFLUENCE ON THE GARDEN ISLAND CAUSEWAY ii Figure 4.1 Transect location _______________________________________________ 33 Figure 4.2 Salinity profiles obtained for Mangles Bay transect at 6.00 AM, 8.00 AM, 10.00 AM and 12.00 noon____________________________________ 34 Figure 4.3 Temperature (degrees Celsius) obtained for Mangles Bay transect at 6.00 AM, 8.00 AM, 10.00 AM and 12.00 noon ___________________________ 35 Figure 4.4 Dissolved oxygen (% saturation) obtained for Mangles Bay transect at 6.00 AM, 8.00 AM, 10.00 AM and 12.00 noon _______________________ 36 Figure 5.1 Changes in dye concentration with different Causeway configurations at selected sites in summer (refined grid) ______________________________ 41 Figure 5.2 Current velocity vectors during a spring tide in summer in the Mangles Bay region: comparison between present Causeway, and doubling of existing Causeway openings ______________________________________ 43 Figure 5.3 Current velocity vectors during a spring tide in summer in the Mangles Bay region: Comparison between present Causeway, and additional Causeway openings _____________________________________________ 44 Figure 5.4 Current velocity vectors during a spring tide in summer in the Mangles Bay region: Comparison between present Causeway configuration, and with the Causeway removed ______________________________________ 44 Figure 5.5 Bottom shear stress during an incoming spring tide in summer (kg/cm/s2), in the absence of the Causeway __________________________ 45 Figure 5.6 Bottom shear stress during an outgoing spring tide in summer (kg/cm/s2), in the absence of the Causeway____________________________________ 46 Figure 5.7 Changes in bottom shear stress (relative to the ‘No Causeway’ configuration) caused by various Causeway configurations: incoming spring tide, summer simulation ____________________________________ 46 Figure 5.8 Changes in bottom shear stress (relative to the ‘No Causeway configuration) caused by various Causeway configurations: outgoing spring tide, summer simulation ____________________________________ 47 Figure 5.9 Refraction of (a) south west and (b) north west swell-waves through South Channel (Modified from FPA, 1972) __________________________ 51 Figure 5.10 Refraction of north east wind-waves through Mangles Bay (Modified from FPA, 1972)._______________________________________________ 52 DALSE:CSMC: INFLUENCE ON THE GARDEN ISLAND CAUSEWAY iii EXECUTIVE SUMMARY Cockburn Sound is a

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