Shore Zone Characterization for Climate Change Adaptation in the Bay of Fundy
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Barriers to Fish Passage in Nova Scotia the Evolution of Water Control Barriers in Nova Scotia’S Watershed
Dalhousie University- Environmental Science Barriers to Fish Passage in Nova Scotia The Evolution of Water Control Barriers in Nova Scotia’s Watershed By: Gillian Fielding Supervisor: Shannon Sterling Submitted for ENVS 4901- Environmental Science Honours Abstract Loss of connectivity throughout river systems is one of the most serious effects dams impose on migrating fish species. I examine the extent and dates of aquatic habitat loss due to dam construction in two key salmon regions in Nova Scotia: Inner Bay of Fundy (IBoF) and the Southern Uplands (SU). This work is possible due to the recent progress in the water control structure inventory for the province of Nova Scotia (NSWCD) by Nova Scotia Environment. Findings indicate that 586 dams have been documented in the NSWCD inventory for the entire province. The most common main purpose of dams built throughout Nova Scotia is for hydropower production (21%) and only 14% of dams in the database contain associated fish passage technology. Findings indicate that the SU is impacted by 279 dams, resulting in an upstream habitat loss of 3,008 km of stream length, equivalent to 9.28% of the total stream length within the SU. The most extensive amount of loss occurred from 1920-1930. The IBoF was found to have 131 dams resulting in an upstream habitat loss of 1, 299 km of stream length, equivalent to 7.1% of total stream length. The most extensive amount of upstream habitat loss occurred from 1930-1940. I also examined if given what I have learned about the locations and dates of dam installations, are existent fish population data sufficient to assess the impacts of dams on the IBoF and SU Atlantic salmon populations in Nova Scotia? Results indicate that dams have caused a widespread upstream loss of freshwater habitat in Nova Scotia howeverfish population data do not exist to examine the direct impact of dam construction on the IBoF and SU Atlantic salmon populations in Nova Scotia. -
A Review of Ice and Tide Observations in the Bay of Fundy
A tlantic Geology 195 A review of ice and tide observations in the Bay of Fundy ConDesplanque1 and David J. Mossman2 127 Harding Avenue, Amherst, Nova Scotia B4H 2A8, Canada departm ent of Physics, Engineering and Geoscience, Mount Allison University, 67 York Street, Sackville, New Brunswick E4L 1E6, Canada Date Received April 27, 1998 Date Accepted December 15,1998 Vigorous quasi-equilibrium conditions characterize interactions between land and sea in macrotidal regions. Ephemeral on the scale of geologic time, estuaries around the Bay of Fundy progressively infill with sediments as eustatic sea level rises, forcing fringing salt marshes to form and reform at successively higher levels. Although closely linked to a regime of tides with large amplitude and strong tidal currents, salt marshes near the Bay of Fundy rarely experience overflow. Built up to a level about 1.2 m lower than the highest astronomical tide, only very large tides are able to cover the marshes with a significant depth of water. Peak tides arrive in sets at periods of 7 months, 4.53 years and 18.03 years. Consequently, for months on end, no tidal flooding of the marshes occurs. Most salt marshes are raised to the level of the average tide of the 18-year cycle. The number of tides that can exceed a certain elevation in any given year depends on whether the three main tide-generating factors peak at the same time. Marigrams constructed for the Shubenacadie and Cornwallis river estuaries, Nova Scotia, illustrate how the estuarine tidal wave is reshaped over its course, to form bores, and varies in its sediment-carrying and erosional capacity as a result of changing water-surface gradients. -
Minas Basin, N.S
An examination of the population characteristics, movement patterns, and recreational fishing of striped bass (Morone saxatilis) in Minas Basin, N.S. during summer 2008 Report prepared for Minas Basin Pulp and Power Co. Ltd. Contributors: Jeremy E. Broome, Anna M. Redden, Michael J. Dadswell, Don Stewart and Karen Vaudry Acadia Center for Estuarine Research Acadia University Wolfville, NS B4P 2R6 June 2009 2 Executive Summary This striped bass study was initiated because of the known presence of both Shubenacadie River origin and migrant USA striped bass in the Minas Basin, the “threatened” species COSEWIC designation, the existence of a strong recreational fishery, and the potential for impacts on the population due to the operation of in- stream tidal energy technology in the area. Striped bass were sampled from Minas Basin through angling creel census during summer 2008. In total, 574 striped bass were sampled for length, weight, scales, and tissue. In addition, 529 were tagged with individually numbered spaghetti tags. Striped bass ranged in length from 20.7-90.6cm FL, with a mean fork length of 40.5cm. Data from FL(cm) and Wt(Kg) measurements determined a weight-length relationship: LOG(Wt) = 3.30LOG(FL)-5.58. Age frequency showed a range from 1-11 years. The mean age was 4.3 years, with 75% of bass sampled being within the Age 2-4 year class. Total mortality (Z) was estimated to be 0.60. Angling effort totalling 1732 rod hours was recorded from June to October, 2008, with an average 7 anglers fishing per tide. Catch per unit effort (Fish/Rod Hour) was determined to be 0.35, with peak landing periods indicating a relationship with the lunar cycle. -
Hydrodynamic Modelling for Flood Management in Bay of Fundy Dykelands”
Hydrodynamic Modelling for Flood Management in Bay of Fundy Dykelands By Michael Fedak A Thesis Submitted to Saint Mary’s University, Halifax, Nova Scotia in Partial Fulfillment of the Requirements for the Degree of Master of Science in Applied Science July 16, 2012, Halifax Nova Scotia © Michael Fedak, 2012 Approved: Dr. Danika van Proosdij Supervisor Department of Geography Approved: Dr. Ryan Mulligan External Examiner Department of Civil Engineering Queen’s University Approved: Dr. Timothy Webster Supervisory Committee Member COGS, NSCC Approved: Dr. Peter Secord Graduate Studies Representative Date: July 16, 2012 Abstract “Hydrodynamic Modelling for Flood Management in Bay of Fundy Dykelands” By Michael Fedak Storm surge in the coastal Bay of Fundy is a serious flood hazard. These lands are low-lying and adapted to farming through the use of coastal defences, namely dykes. Increasing rates of sea level rise due to climate change are expected to increase flood hazard in this area. In this thesis, flood risk to communities in the Avon River estuary of the Upper Bay of Fundy is investigated through computer based modelling and data management techniques. Flood variables from 14 possible storm surge scenarios (based on sea level rise predictions) were modelled using TUFLOW software. A GIS was used to create a database for simulation outputs and for the analysis of outputs. TUFLOW and a geographic information system (GIS) flood algorithm are compared .It was found that obstructions to flow controlled flooding and drainage and these features required the use of a hydrodynamic model to represent flows properly. July 16, 2012 2 Acknowledgements Funding Sources: • Atlantic Canada Adaptation Solutions Association part of the Natural Resources Canada Regional Adaptation Collaboratives (RAC) Project. -
Sedimentation in the Inner Cornwallis Estuary, Minas Basin, Nova
166 ABSTRACTS Sedimentation in the inner Cornwallis F.stuary, Minas Basin, Nova Scotia: implications for contaminant accumulation G. Yeo, E. Bishop, A. Dickinson Department of Geology, Acadia University, Wolfville, Nova Scotia BOP JXO, Canada and R. Faas Department of Geology, Lafayette College, Easton, Pennsylvania 18042, U.SA. The estuary of the Cornwallis River is a macrotidal system Salmon River estuary. Compared to the latter, it is mud-domi within the Minas Basin, like the better-known Cobequid Bay - nated. Tidal range and flow conditions are highly variable: Atlantic Geology, July 1991, Volume 27, Number 2 Copyright © 2015 Atlantic Geology ATLANTIC GEOLOOY 167 Site: Port New Kent ville plane or rippled, silty beds are interbedded with water-saturated Williams Minas clays deposited at slack water. Overpressure conditions resulting Spring tide range (m): 12.15 4.1 2.15 from the ebb of overlying waters produce numerous fluidization Max. velocity (cm/s): 177 132 83 features. Min. velocity (cm/s}: 58 29 21 Except where the river has cut into Triassic sandstone, the banks are dyked and locally faced with rip-rap. Along most of Except at slack water, when suspended sediment settles out their length they are mud, deposited from suspension, and inten rapidly the water column is well-mixed. Suspended sediment sively gullied. Bank mud deposits are continuously recycled to concentration varies from 50 mg/I near Wolfville to >4.5 g/l at the river by fluidized flow, scouring, or undercutting and slump the turbidity maximum between New Minas and Kentville. ing. Seeps and springs are common along the banks at low water. -
Nova Scotia Inland Water Boundaries Item River, Stream Or Brook
SCHEDULE II 1. (Subsection 2(1)) Nova Scotia inland water boundaries Item River, Stream or Brook Boundary or Reference Point Annapolis County 1. Annapolis River The highway bridge on Queen Street in Bridgetown. 2. Moose River The Highway 1 bridge. Antigonish County 3. Monastery Brook The Highway 104 bridge. 4. Pomquet River The CN Railway bridge. 5. Rights River The CN Railway bridge east of Antigonish. 6. South River The Highway 104 bridge. 7. Tracadie River The Highway 104 bridge. 8. West River The CN Railway bridge east of Antigonish. Cape Breton County 9. Catalone River The highway bridge at Catalone. 10. Fifes Brook (Aconi Brook) The highway bridge at Mill Pond. 11. Gerratt Brook (Gerards Brook) The highway bridge at Victoria Bridge. 12. Mira River The Highway 1 bridge. 13. Six Mile Brook (Lorraine The first bridge upstream from Big Lorraine Harbour. Brook) 14. Sydney River The Sysco Dam at Sydney River. Colchester County 15. Bass River The highway bridge at Bass River. 16. Chiganois River The Highway 2 bridge. 17. Debert River The confluence of the Folly and Debert Rivers. 18. Economy River The highway bridge at Economy. 19. Folly River The confluence of the Debert and Folly Rivers. 20. French River The Highway 6 bridge. 21. Great Village River The aboiteau at the dyke. 22. North River The confluence of the Salmon and North Rivers. 23. Portapique River The highway bridge at Portapique. 24. Salmon River The confluence of the North and Salmon Rivers. 25. Stewiacke River The highway bridge at Stewiacke. 26. Waughs River The Highway 6 bridge. -
They Planted Well: New England Planters in Maritime Canada
They Planted Well: New England Planters in Maritime Canada. PLACES Acadia University, Wolfville, Nova Scotia, 9, 10, 12 Amherst Township, Nova Scotia, 124 Amherst, Nova Scotia, 38, 39, 304, 316 Andover, Maryland 65 Annapolis River, Nova Scotia, 22 Annapolis Township, Nova Scotia, 23, 122-123 Annapolis Valley, Nova Scotia, 10, 14-15, 107, 178 Annapolis County, Nova Scotia, 20, 24-26, 28-29, 155, 258 Annapolis Gut, Nova Scotia, 43 Annapolis Basin, Nova Scotia, 25 Annapolis-Royal (Port Royal-Annapolis), 36, 46, 103, 244, 251, 298 Atwell House, King's County, Nova Scotia, 253, 258-259 Aulac River, New Brunswick, 38 Avon River, Nova Scotia, 21, 27 Baie Verte, Fort, (Fort Lawrence) New Brunswick, 38 Barrington Township, Nova Scotia, 124, 168, 299, 315, Beaubassin, New Brunswick (Cumberland Basin), 36 Beausejour, Fort, (Fort Cumberland) New Brunswick, 17, 22, 36-37, 45, 154, 264, 277, 281 Beaver River, Nova Scotia, 197 Bedford Basin, Nova Scotia, 100 Belleisle, Annapolis County, Nova Scotia, 313 Biggs House, Gaspreau, Nova Scotia, 244-245 Blomidon, Cape, Nova Scotia, 21, 27 Boston, Massachusetts, 18, 30-31, 50, 66, 69, 76, 78, 81-82, 84, 86, 89, 99, 121, 141, 172, 176, 215, 265 Boudreau's Bank, (Starr's Point) Nova Scotia, 27 Bridgetown, Nova Scotia, 196, 316 Buckram (Ship), 48 Bucks Harbor, Maine, 174 Burton, New Brunswick, 33 Calkin House, Kings County, 250, 252, 259 Camphill (Rout), 43-45, 48, 52 Canning, Nova Scotia, 236, 240 Canso, Nova Scotia, 23 Cape Breton, Nova Scotia, 40, 114, 119, 134, 138, 140, 143-144 2 Cape Cod-Style House, 223 -
Upgrading the Avon River Causeway During Highway 101 Twinning
Upgrading the Avon River Causeway During Highway 101 Twinning Dr. Bob Pett, NSTIR Environmental Services Alexander Wilson, CBCL Limited Transportation and Infrastructure Renewal Partner with NS Agriculture 9.5 km 6 lanes PEI Moncton NB Northumberland Strait Petitcodiac River NS Chignecto Bay Minas Basin Bay of Fundy Avon River Windsor Fundy Tides Salty- Silty Lake Pesaquid 1970 Fresh water Impacts on the Windsor Salt Marsh (Ramsar Wetland & IBA of Canada) Unlike the Petitcodiac – keeping an aboiteau EA completed in 2017 – currently working on design Project in planning for almost 20 years – including various environmental studies of the Avon River Estuary Contracted Acadia University, St. Mary’s University and CBWES Inc., between 2002 and 2018 to better understand the estuary and inform our design team to minimize impacts on salt marsh and mudflats. Baseline CRA Fisheries Study (Commercial, Recreational and Aboriginal) Contracted 3 partners for work between April 2017 and March 2019 ➢ Darren Porter, commercial fisher, ➢ Acadia University (Dr. Trevor Avery) ➢ Mi’kmaq Conservation Group Key study goal to better inform the detailed design team to improve fish passage through the aboiteau (sluice) Just before Christmas 2017, we engaged a team led by CBCL Limited to design an upgraded causeway and aboiteau system. Design Objectives Public Safety • Maintain corridor over Avon River for Highway 101 Twinning and continuity of rail, trail and utility services. • Continued protection of communities and agricultural land from the effects of flooding and sea level rise / climate change. Regulatory Requirements • Improve fish passage (EA Condition & Fisheries Act ). • Minimize environmental impacts (i.e., impact to salt marsh). • Consideration of potential negative impacts to asserted or established Mi’kmaq aboriginal or treaty rights. -
Support for Delineation of Inner Bay of Fundy Salmon Marine Critical Habitat Boundaries in Minas Basin and Chignecto
Canadian Science Advisory Secretariat Maritimes Region Science Response 2015/035 SUPPORT FOR DELINEATION OF INNER BAY OF FUNDY SALMON MARINE CRITICAL HABITAT BOUNDARIES IN MINAS BASIN AND CHIGNECTO BAY Context In April 2014, the Fisheries and Oceans Canada (DFO) Species at Risk Management Division (SARMD) in the Maritimes Region requested information from DFO Science to assist with the delineation of boundaries for critical habitat (CH) being considered for Inner Bay of Fundy (IBOF) Atlantic Salmon within Chignecto Bay and Minas Basin, specifically: to assist with the delineation of the boundary between estuarine and marine habitat for several large, tidal estuaries (i.e., Petitcodiac River, Avon River, Salmon River Colchester, Shubenacadie River estuary and Cumberland Basin). DFO Science had previously provided advice on the characteristics and general location of important marine and estuarine habitat for IBOF salmon (DFO 2008; DFO 2013); however, additional information was requested to assist in delineating the precise boundaries of important marine habitat within Chignecto Bay and Minas Basin in order to subsequently propose, describe and map these as CH within an amended Recovery Strategy for IBOF salmon. Once identified in the Recovery Strategy, measures will be taken to protect this marine CH under the Species at Risk Act (SARA). This Science Response Report results from the Science Response Process of 11 July 2014 on Support for Delineation of Inner Bay of Fundy Salmon Marine Critical Habitat Boundaries. Background The inner Bay of Fundy populations of Atlantic salmon (Salmo salar) are listed as Endangered under the Species at Risk Act, and SARA requires the identification of CH for endangered species within a Recovery Strategy (or Action Plan). -
Seasonal Variability of Total Suspended Matter in Minas Basin, Bay of Fundy
SEASONAL VARIABILITY OF TOTAL SUSPENDED MATTER IN MINAS BASIN, BAY OF FUNDY by Jing Tao Submitted in partial fulfilment of the requirements for the degree of Master of Science at Dalhousie University Halifax, Nova Scotia July 2013 © Copyright by Jing Tao, 2013 For my parents, who encouraged me all the way long. I love them forever. ii TABLE OF CONTENTS LIST OF TABLES .............................................................................................................. v LIST OF FIGURES ........................................................................................................... vi ABSTRACT ................................................................................................................ viii LIST OF ABBREVIATIONS AND SYMBOLS USED ................................................... ix ACKNOWLEDGEMENTS ............................................................................................... xi CHAPTER 1 INTRODUCTION ..................................................................................... 1 1.1 Background ........................................................................................................... 1 1.2 Geology of Minas Basin ....................................................................................... 2 1.3 Literature Review .................................................................................................. 4 1.3.1 Point Measurements ....................................................................................... 4 1.3.2 Satellite Measurements -
Environmental Implications of Expanding the Windsor Causeway (Part 2)
Environmental Implications of Expanding the Windsor Causeway (Part 2): Comparison of 4 and 6 Lane Options Final Report prepared for Nova Scotia Department of Transportation and Public Works ACER Report No. 75 2 Environmental Implications of Expanding the Windsor Causeway (Part 2): Comparison of 4 and 6 Lane Options Report Prepared for Nova Scotia Department of Transportation and Public Works. Contract # 02-00026 Prepared by Danika van Proosdij, Graham R. Daborn and Michael Brylinsky April 2004. 3 1.0 Introduction Preliminary plans for twinning Highway 101 include expansion of the width of the Windsor Causeway to accommodate two or four additional lanes, creating a four or six lane divided highway. Because of the limitations imposed by infrastructure in the Town of Windsor, and by Fort Edward, such expansion is feasible only on the seaward side of the existing structure. Realignment of the existing roadway would also be designed to decrease the sharp curve at the western end, which currently requires a speed limit of 90 km per hour. The new construction would therefore cover part of the marsh and tidal channel adjacent to the existing causeway. During 2002, studies of the mudflat—saltmarsh complex on the seaward side of the Windsor Causeway and of Pesaquid Lake, were carried out, in part, to provide information relevant to an assessment of the ecological implications of such an expansion. These studies also constituted the first step in a planned long term monitoring of continuing evolution of the marsh-mudflat complex that has resulted from construction of the original causeway. Reports on the 2002 studies were presented as ACER Publications 69 and 72 in 2003 (Daborn et al. -
Retour En Acadie
Preface References “…it was a Fine Country and Full of Inhabitants, Modern Placenames Old Placenames a Butiful Church & abundance of ye Goods of the world. Annapolis River Rivière Dauphin Paradise Paradis Terrestre Provisions of all kinds in great Plenty.” Melanson Settlement Établissement Melanson Lt. Col. John Winslow, September 3, 1755 Round Hill Prée Ronde Cornwallis River Rivière Saint Antoine/ Rivière Grand Habitant This guide is for people who want to deepen their understanding and Canard Rivière aux Canards appreciation of Acadian history by exploring the AnnapolisValley of Nova Porters Point Pointe des Breau Scotia through “Acadian eyes.” Minas Basin Bassin des Mines Starrs Point Côte des Boudreau/ Petite Côte/ It contains information which was collected from primary documents, printed Pointe des Boudreau/ works or expert testimony. This information has never been found in one document before. Régis Brun's book Les Acadiens avant 1755 helped to give a Village des Michel human face to the 17th and 18th century Acadians. Lt. Col. John Winslow's New Minas Rivière des Habitants Journal was more interesting and educational each time I read it and some of Canning/ Pereau/ Kingsport Rivière des Vieux Habitants the primary documents were sobering. Habitant River Rivière de la Veille Habitation Pereaux River Rivière Pereau Inside, you will find geographical locations in the beautiful AnnapolisValley that Grand-Pré Les Mines/ Grand-Pré have significance in Acadian history. It also includes some of the Acadian family names connected to many of these locations. I have made every effort Horton Landing Pointe Noire/ Vieux Logis to be historically accurate. However, the guide is far from being complete.