The Oceanographic Circulation of the Port of Saint John Over Seasonal and Tidal Time Scales
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THE OCEANOGRAPHIC CIRCULATION OF THE PORT OF SAINT JOHN OVER SEASONAL AND TIDAL TIME SCALES by Reenu Toodesh BSc. Surveying and Land Information, University of the West Indies, St. Augustine, 2007 A Thesis Submitted in Partial Fulfillment of the Requirements for the Degree of Master of Science in Engineering in the Graduate Academic Unit of Geodesy and Geomatics Enginering Supervisor: John Hughes Clarke, PhD., Geodesy and Geomatics Engineering Examining Board: Susan Nichols, PhD., Geodesy and Geomatics Engineering Susan Haigh, PhD., Geodesy and Geomatics Engineering Katy Haralampides, PhD., Civil Engineering This thesis is accepted by the Dean of Graduate Studies THE UNIVERSITY OF NEW BRUNSWICK April, 2012 ©Reenu Toodesh, 2012 ABSTRACT As part of the sustainable management of the Port of Saint John there is a critical need to maintain sufficient under keel clearance for the various container and cruise ship traffic in and out of the harbour. Because of high and variable sedimentation rates, annual maintenance dredging is necessary and causes economic concerns for the Port. Therefore to better predict future dredging volumes and hence improve the budgeting process for the Port of Saint John, the estuarine circulation of the harbour has been analysed to better quantify the relative importance of the offshore sediments that contribute to the high dredging volumes in the Saint John harbour. The Port of Saint John lies at the mouth of the Saint John River on the north side of the macrotidal Bay of Fundy. Because of this, the harbour sedimentation is influenced by two major sources of siltation: the Saint John River and the Bay of Fundy. The sediment flux from the river is strongly modulated by the seasonal variations in river discharge. In the Bay of Fundy, there is significant resuspension of offshore marine sediments. To better understand this complex interaction between the fresh water flow and the tidal inflow of salt water, high density oceanographic surveys have been conducted at four different river discharge periods. In order to quantitatively analyse the mixing of the fresh and salt water in the harbour channels, high density ADCP currents and CTD measurements were acquired along main longitudinal axis of the Main Harbour channel and Courtenay Bay over four tidal cycles. By imaging the 200kHz acoustic volume backscatter within the water column, the appearance of interfacial waves at the ii pycnocline can be examined. The optical backscatter sensor provided observations used to estimate suspended sediment concentrations. A cross-sectional analysis of the flow at a location 700m south and seaward of the Rodney bay terminal in the Main Channel revealed that regardless of the river discharge rate, the interfacial waves are best developed on the rising tide. However, during the Spring freshet the interfacial waves are also developed at high tide, low tide and falling tide. Examination of the timing and location of the interfacial waves are important because they influence the nature of sediment transport in the Main Harbour Channel. During high river discharge periods, the sediment concentration and volume flux estimates indicate that the river is the main source of sediments. For the low river discharge periods, the observations suggest that the possible source of suspended sediments observed in the lower saline layer are either from outside of the harbour or bottom sediments being resuspended on the rising tide. iii ACKNOWLEDGEMENTS I am truly grateful for the opportunity to thank some people who helped me successfully complete this research project. I am very appreciative for the funding received for this research provided by NSERC and my supervisor, the Chair of the Ocean Mapping group, Dr. John Hughes Clarke. I cannot express enough how thankful I am him for allowing me this project. I thank you for your enthusiasm, inspiration, patience and continuous efforts in taking the time to explain the oceanography concepts for me. I would not have been able to do it without your invaluable direction. I would also like to thank Dr. Susan Haigh for taking the time to answer any questions about mathematical concepts whether it was used or not during my research. A special thanks to many members of the Ocean Mapping Group; the Heron Specialist, Steve Brucker, for assisting me in the operations of all equipment used to collect the much needed data in this study. To Ian Church, Doug Cartwright and James Muggah I also thank you for your support. Titus Tienaah, I am very grateful for you being my programming guru at times. Last and most importantly I would like to thank my family, Toodesh Ramesar and Nina Toodesh, for your encouragement, financial assistance and love. To my sisters, Vida and Simi I hope I can now join you on your travels. Hamid, you are my joy, thanks for your continuous encouragement. iv TABLE OF CONTENTS ABSTRACT .............................................................................................................. ii ACKNOWLEDGEMENTS ...................................................................................... iv TABLE OF CONTENTS ........................................................................................... v LIST OF TABLES .................................................................................................. viii LIST OF FIGURES .................................................................................................. ix Chapter 1: INTRODUCTION – RESEARCH INTEREST ............................................. 1 1.1 Research Objectives ............................................................................................. 3 Chapter 2: STUDY AREA ............................................................................................. 4 2.1. Description of the Study area –Location and description of Saint John Harbour .. 4 2.2 Offshore Wave and Climate Study ..................................................................... 10 2.3 Water Levels, Tides and River Discharge ........................................................... 13 2.3.1 Tidal Influence in the Saint John Harbour study area ................................... 13 2.3.2 River Discharge ........................................................................................... 14 2.3.3 River Water levels for the Oceanographic Surveys of the Saint John Harbour ............................................................................................................................. 16 2.3.4 Wind and Wave Activities affecting the Saint John Harbour ........................ 20 2.4 Siltation processes in the harbour ....................................................................... 22 Chapter 3: ESTUARINE CIRCULATION AND SEDIMENTATION CONTROL ...... 27 3.1 Review of the characteristics of the Saint John Estuarine System ....................... 27 3.1.1 The Reversing Falls ..................................................................................... 29 3.1.2 Kennebacasis Bay ........................................................................................ 30 3.1.3 Estuarine characteristics of the Saint John Harbour ...................................... 31 3.2 Measurements of Turbulent Mixing in Estuaries ................................................. 37 3.2.1 Richardson number (Ri)............................................................................... 37 3.3 Controls on suspension and deposition of cohesive sediments. ........................... 39 3.4 Characteristics of the plume of the Saint John River ........................................... 40 v Chapter 4: Survey Instrumentation and Methodology ................................................... 46 4.1 Principles of the Acoustic Doppler Current Profiler (RDI Workhorse Monitor 600kHz) ................................................................................................................... 46 4.1.1 Depth Cell (Bin Size) and Range Gate ......................................................... 48 4.1.2 Bottom Tracking of the ADCP .................................................................... 49 4.1.3 Limitations of using the ADCP for current measurements............................ 50 4.3 Moving Vessel Profiler with CTD sensors .......................................................... 53 4.3.1 Optical Backscatter ...................................................................................... 57 4.4 Knudsen 320 B/P 200 kHz echo sounder ............................................................ 58 4.5 Quantification of Volumetric Fluxes: Freshwater flux, Saltwater flux and Sediment Flux .......................................................................................................... 59 4.5.1 Calculations for Fluxes ................................................................................ 60 4.5.2 Calculation for the Gradient Richardson Number ......................................... 66 Chapter 5: RESULTS AND ANALYSIS ..................................................................... 68 5.1. Main Harbour Channel Oceanographic Results ................................................. 68 5.2 Tidal Cycle - Winter minimum discharge (March 2009) ..................................... 71 5.2.1 Zoom of the 200kHz acoustic imagery of the halocline during the winter minimum observations. ........................................................................................ 74 5.2.3 Velocity and Density Structure at the cross-section location. ....................... 76