Volume Two of the Current Tides Magazine
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Based Circulation Model for the Mid-Atlantic Bight and Gulf of Maine: Configuration and Comparison to Integrated Coastal Observing Network Observations
Geosci. Model Dev., 13, 3709–3729, 2020 https://doi.org/10.5194/gmd-13-3709-2020 © Author(s) 2020. This work is distributed under the Creative Commons Attribution 4.0 License. Doppio – a ROMS (v3.6)-based circulation model for the Mid-Atlantic Bight and Gulf of Maine: configuration and comparison to integrated coastal observing network observations Alexander G. López, John L. Wilkin, and Julia C. Levin Department of Marine and Coastal Sciences, Rutgers, The State University of New Jersey, New Brunswick, NJ 08901, United States of America Correspondence: Alexander G. López ([email protected]) Received: 20 December 2019 – Discussion started: 4 March 2020 Revised: 16 June 2020 – Accepted: 8 July 2020 – Published: 24 August 2020 Abstract. We describe “Doppio”, a ROMS-based (Regional sediments, or pollutants. The reduced geographic scope of Ocean Modeling System) model of the Mid-Atlantic Bight a regional model offers economies in computational effort and Gulf of Maine regions of the northwestern North Atlantic that allow much greater experimentation than would be pos- developed in anticipation of future applications to biogeo- sible with global models alone, such as by examining sen- chemical cycling, ecosystems, estuarine downscaling, and sitivity to resolution or parameterization of added physics, near-real-time forecasting. This free-running regional model and they present the opportunity to affordably explore nu- is introduced with circulation simulations covering 2007– merous application scenarios. Here we describe the develop- 2017. The ROMS configuration choices for the model are ment, evaluation, and application of a regional model of the detailed, and the forcing and boundary data choices are de- northeastern continental shelf of North America from Cape scribed and explained. -
It Has Often Been Said That Studying the Depths of the Sea Is Like Hovering In
It has often been said that studying the depths of the sea is like hovering in a balloon high above an unknown land which is hidden by clouds, for it is a peculiarity of oceanic research that direct observations of the abyss are impracticable. Instead of the complete picture which vision gives, we have to rely upon a patiently put together mosaic representation of the discoveries made from time to time by sinking instruments and appliances into the deep. (Murray & Hjort, 1912: 22) Figure 1: Portrait of the H.M.S. Challenger. Prologue: Simple Beginnings In 1872, the H.M.S Challenger began its five- year journey that would stretch across every ocean on the planet but the Arctic. Challenger was funded for a single reason; to examine the mysterious workings of the ocean below its surface, previously unexplored. Under steam power, it travelled over 100,000 km and compiled 50 volumes of data and observations on water depth, temperature and conditions, as well as collecting samples of the seafloor, water, and organisms. The devices used to collect this data, while primitive by today’s standards and somewhat imprecise, were effective at giving humanity its first in-depth look into the inner workings of the ocean. By lowering a measured rope attached to a 200 kg weight off the edge of the ship, scientists estimated the depth of the ocean. A single reading could take up to 80 minutes for the weight to reach bottom. Taking a depth measurement also necessitated that the Challenger stop moving, and accurate mapping required a precise knowledge of where the ship was in the world, using navigational tools such as sextants. -
David Moretti Phd Thesis
ESTIMATING THE EFFECT OF MID-FREQUENCY ACTIVE SONAR ON THE POPULATION HEALTH OF BLAINVILLE'S BEAKED WHALES (MESOPLODON DENSIROSTRIS) IN THE TONGUE OF THE OCEAN David Moretti A Thesis Submitted for the Degree of PhD at the University of St Andrews 2019 Full metadata for this item is available in St Andrews Research Repository at: http://research-repository.st-andrews.ac.uk/ Please use this identifier to cite or link to this item: http://hdl.handle.net/10023/19250 This item is protected by original copyright Estimating the effect of mid-frequency active sonar on the population health of Blainville's beaked whales (Mesoplodon densirostris) in the Tongue of the Ocean David Moretti This thesis is submitted in partial fulfilment for the degree of Doctor of Philosophy (PhD) at the University of St Andrews March 2019 Abstract Passive acoustic methods were used to study the effect of mid-frequency active sonar (MFAS) on a population of Blainville’s beaked whales (Mesoplodon densirostris, Md) at the U.S. Navy Atlantic Undersea Test and Evaluation Centre (AUTEC), Bahamas. AUTEC contains an array of bottom-mounted hydrophones that can detect Md echolocation clicks. Methods to estimate abundance, the risk of behavioural disruption, and the population level effect of repeated MFAS exposure are presented. A passive acoustic abundance estimation method, a parametric equation that predicts the probability of foraging dive disruption as a function of MFAS received level and an Md bioenergetics model were developed. The effect of changes in energy flow on the demographic characteristics of an Md population were explored. Passive acoustic data from AUTEC were used to estimate the behavioural disturbance resulting from sonar operations; combined with the bioenergetic model, this suggested that the effect of sonar operations could cause an increase in a female’s age at maturity, a longer inter-calf-interval, calf survival rate and probability of giving birth that could in turn result in a declining population. -
A Geological History of Southwestern Nova Scotia - C
CH MINING RAN MATTERS B REPORT ME 2004-2 2004 ED. D. R. MACDONALD ESOURCES ALR INER THE WESTIN NOVA SCOTIAN HOTEL NOVEMBER 1 AND 2, 2004 M Natural Resources Honourable Richard Hurlburt Minister Peter Underwood Deputy Minister Halifax, Nova Scotia 2004 019621 ii CONTENTS Program ....iv Peat Resources of Southwestern Nova Scotia - A. R. Anderson ....1 The Callie Lode Gold Deposit, Northern Territory, Australia: High- grade, Sheeted, Auriferous Quartz Veins in an Anticlinal Structural Environment - J. Bigelow and C. R. Stanley .....2 Geology and Economic Potential of Upper Carboniferous Rocks in Nova Scotia: Tradition Meets Innovation - J. H. Calder ..... 3 A Comparison of the Late Triassic Dinosaur Footprints Atreipus acadianus and Grallator (Grallator) sp. from the Upper Wolfville Formation at North Medford, Nova Scotia - B. Cameron and N. Wood ...4 A Geological and Geophysical Study of the Large, Positive Magnetic Anomaly between Eastern Prince Edward Island and Western Cape Breton Island, Nova Scotia - L. Cook, S. M. Barr and S. Dehler ....5 The Story of Halifax Harbour - G. B. J. Fader ..... 6 Recent Advances in the Geology of the Windsor Group in Nova Scotia - P. S. Giles ... 7 Update on the Bedrock Mapping Component of the Targeted Geoscience Initiative (Phase 2) - P. S. Giles, R. D. Naylor and D. C. Brisco ....8 Nova Scotia Gold Grain Study: Background Concentrations and Distance of Transport - T. A. Goodwin ...... 9 Regional and Detailed Geochemical Sampling of Humus, Soil and Till in the Upper and Lower Seal Harbour Gold Districts - T. A. Goodwin . .... 10 Regional Humus, Soil and Till Sampling for the Targeted Geoscience Initiative (Phase 2) - T. -
Offshore/ Continental Shelf
................ ............................ ... PAGE 227... Offshore/ Continental Shelf 68' 67' 66 56' 48 65 64 63 62 "7' 47• a,_L~so ~~ ~ 46' 45' .... 45' 44' t----1-=...~ ~-r ·.. I "--,- 1· I 44' 43' L_~ L.-----1 43' 42' r----\. I I h~ / L I I 42' ---+ - . I I .,c::;{§)r- 7 · I I 41 ° r f ......~ fUI IUII:JIIVIII;Jllflf:l l , /"1f''' I __, 41 ' ) \ -J:J----+--- ""' .I f 40' - 40' 68' 67' 66' --.L... 65 57' 55• 55' 54' 64 63 62 61 60' 59' 58' Figure 30: Region 900, Offshore/Continental Shelf, and its component Districts, Units. and sub-Units. Theme Regions: Natural History of Nova Scotia, Vo lume II PAGE • • •• 0 • 0 • • • 0 •••• • •••• 0 . 0 •• 0 0 • • ••• 0 • ••• 0 ••• 0 • • 0 •• • • • 0 0 0 228 900 OFFSHORE/ CONTINENTAL SHELF The following physiographic features are the basis fo r form ations on the adjacent lan d. Areas of complex the d ivision of the Districts of Region 900: geology may have different subtidal bedrock than on • District 910, Inner Shelf, is a zone of gradually the coast. Patterns and variations of bed rock geology sloping bottom adjacen t to sho re and extending are not as easily identified in the offshore but are to depths of about II 0 metres in all areas probably as varied as on land. • District 920, Middle Shelf, is a zone of fi shing Four major geological or bedrock u nits are repre banks and deep basins in the mid-portions of sented: (l) the Acadian Basin, an area of Triassic the continental shelf and includes the Scotian rocks in tl1e Bay of Fundy and northern Gulf of Shelf and the Gulf of Maine Maine, -
Acoustic Cymbal Transducers-Design, Hydrostatic Pressure Compensation, and Acoustic Performance
Calhoun: The NPS Institutional Archive DSpace Repository Theses and Dissertations 1. Thesis and Dissertation Collection, all items 2004-03 Acoustic cymbal transducers-design, hydrostatic pressure compensation, and acoustic performance Jenne, Kirk E. Monterey, California. Naval Postgraduate School http://hdl.handle.net/10945/1670 Downloaded from NPS Archive: Calhoun NAVAL POSTGRADUATE SCHOOL MONTEREY, CALIFORNIA THESIS ACOUSTIC CYMBAL TRANSDUCERS – DESIGN, HYDROSTATIC PRESSURE COMPENSATION, AND ACOUSTIC PERFORMANCE by Kirk E. Jenne March 2004 Thesis Advisor: Thomas R. Howarth Thesis Co-Advisor: Dehua Huang Approved for public release; distribution unlimited THIS PAGE INTENTIONALLY LEFT BLANK REPORT DOCUMENTATION PAGE Form Approved OMB No. 0704-0188 Public reporting burden for this collection of information is estimated to average 1 hour per response, including the time for reviewing instruction, searching existing data sources, gathering and maintaining the data needed, and completing and reviewing the collection of information. Send comments regarding this burden estimate or any other aspect of this collection of information, including suggestions for reducing this burden, to Washington headquarters Services, Directorate for Information Operations and Reports, 1215 Jefferson Davis Highway, Suite 1204, Arlington, VA 22202-4302, and to the Office of Management and Budget, Paperwork Reduction Project (0704-0188) Washington DC 20503. 1. AGENCY USE ONLY (Leave blank) 2. REPORT DATE 3. REPORT TYPE AND DATES COVERED March 2004 Master’s Thesis 4. TITLE AND SUBTITLE: Acoustic Cymbal Transducers – Design, 5. FUNDING NUMBERS Pressure Compensation, and Acoustic Performance 6. AUTHOR(S) Kirk E. Jenne 7. PERFORMING ORGANIZATION NAME(S) AND ADDRESS(ES) 8. PERFORMING Naval Postgraduate School ORGANIZATION REPORT Monterey, CA 93943-5000 NUMBER 9. -
Convoy Cup Mini-Offshore Race September 12, 2020
Notice of Race Convoy Cup Mini-Offshore Race September 12, 2020 1. Organizing Authority: These races are hosted by the Dartmouth Yacht Club of Dartmouth, Nova Scotia. 2. Objectives: The Convoy Cup Ocean Race offers racing and cruising yachts an opportunity to participate in an ocean race to commemorate the links that formed between the province of Nova Scotia and the countries of Europe during the two world wars. Halifax was the congregation point for hundreds of naval vessels and supply ships that formed convoys to transport the necessities of life across the Atlantic Ocean; this race is dedicated to the memory of all those men and women in the navy and merchant marine service who sailed in those convoys. 3. Rules: Racing will be governed by the Racing Rules of Sailing 2017-2020 (RRS), the prescriptions of the Canadian Yachting Association and this Notice of Race except as modified by the Sailing Instructions. Dartmouth Yacht Club Race Committee (RC) will have final authority on all matters. 4. Description: Normally the Convoy Cup is an overnight 100 n/m ocean race and a Basin Race is also held. This season is quite different due to the COVID 19 pandemic so the event this year has been changed to a mini-offshore race. The Convoy Cup Mini-Offshore Race will be comprised of 1 race of approximately 30 n/m (course and distances may be adjusted according to forecast winds and conditions). 5. Start date, course and finish: The races will commence September 12, 2020 at 1200 at a start line established between the Navy Island buoy HY2 (Mark 11on the DYC course card) and the RC flag on the Race Committee boat passing either side of George’s Island outbound only, and proceeding to HB, port rounding and return keeping George’s Island to starboard, to finish at the CSS Acadia dock, at in a line projected from the edge of the wharf, which is closest to the Last Steps Memorial. -
Riparian Buffer Removal and Associated Land Use in the Sackville River Watershed, Nova Scotia, Canada
Riparian Buffer Removal and Associated Land Use in the Sackville River Watershed, Nova Scotia, Canada Submitted for ENVS 4901/4902 - Honours April 5, 2010 Supervisor: Shannon Sterling By Emily Rideout 0 Abstract “To what extent has riparian area been removed in the Sackville River watershed and what land uses are associated with this riparian area removal?” I investigate this question by assessing the extent of riparian area removal in the Sackville River watershed north of Halifax and characterizing each riparian impact zone with the neighbouring land use. Stream, lake and road data and air photographs are used in Geographic Information Systems (GIS) to document the degree of riparian area removal and the land uses associated with the riparian area (agriculture, industry, forestry, residential etc). I consider the riparian area to be a 20m zone extending from the water body’s edge. Over 143km of streams are assessed and all streams are broken down into reaches of discrete lengths based on riparian impact and land use category. Four qualitative indicators of riparian removal are used: Severe, Moderate, Low and Intact. The length of every reach as well as the degree of impact and associated land use are calculated using the summary statistics function in GIS. I found that one third of the total riparian area length is missing up to 50% of its vegetation and that residential, transportation and energy infrastructure were the leading drivers of this riparian buffer removal. I present a map of impacted riparian “hot spots” that will highlight the areas in which riparian area removal is the most severe as well as summaries of the land uses most associated with the greatest degree of riparian vegetation removal. -
Using the Δ18 O-Salinity Relationship to Identify
USING THE δ18O-SALINITY RELATIONSHIP TO IDENTIFY FRESHWATER INPUTS TO A NORTH ATLANTIC ESTUARY by Elizabeth Kerrigan Submitted in partial fulfillment of the requirements for the degree of Master of Science at Dalhousie University Halifax, Nova Scotia March 2015 © Copyright by Elizabeth Kerrigan, 2015 To my family, my friends, and my love; I am forever grateful for your support. Thank you for following me down this long and winding road. ii TABLE OF CONTENTS List of Tables ..................................... v List of Figures .................................... vii Abstract ........................................ xi List of Abbreviations and Symbols Used ...................... xii Acknowledgements ................................. xiii Chapter 1 Introduction ............................ 1 1.1 Motivation .................................. 1 1.2 Water Mass Analysis ............................ 2 1.2.1 Introduction to Stable Isotopes ................... 2 1.2.2 Isotope Fractionation in Water ................... 3 1.2.3 Tracing 18O through the Hydrological Cycle ............ 6 1.2.4 δ18O-Salinity Relationship ..................... 8 1.3 Oceanographic Setting of Halifax Harbour and its Approaches ...... 10 1.3.1 Halifax Harbour .......................... 10 1.3.2 Scotian Shelf ............................ 19 1.4 Objectives .................................. 21 Chapter 2 Methods ............................... 23 2.1 Field Sites .................................. 23 2.1.1 Halifax Harbour .......................... 23 2.1.2 Scotian Shelf ........................... -
Fishery Bulletin of the Fish and Wildlife Service V.53
'I', . FISRES OF '!'RE GULF OF MAINE. 101 Description.-The hickory shad differs rather Bay, though it is found in practically all of them. noticeably from the sea herring in that the point This opens the interesting possibility that the of origin of its dorsal fin is considerably in front of "green" fish found in Chesapeake Bay, leave the the mid-length of its trunk; in its deep belly (a Bay, perhaps to spawn in salt water.65 hickory shad 13~ in. long is about 4 in. deep but a General range.-Atlantic coast of North America herring of that length is only 3 in. deep) ; in the fact from the Bay of Fundy to Florida. that its outline tapers toward both snout and tail Occurrence in the Gulf oj Maine.-The hickory in side view (fig. 15); and in that its lower jaw shad is a southern fish, with the Gulf of Maine as projects farther beyond the upper when its mouth the extreme northern limit to its range. It is is closed; also, by the saw-toothed edge of its belly. recorded in scientific literature only at North Also, it lacks the cluster of teeth on the roof of the· Truro; at Provincetown; at Brewster; in Boston mouth that is characteristic of the herring. One Harbor; off Portland; in Casco Ba3T; and from the is more likely to confuse a hickory shad with a shad mouth of the Bay of Fundy (Huntsman doubts or with the alewives, which it resembles in the this record), and it usually is so uncommon within position of its dorsal fin, in the great depth of its our limits that we have seen none in the Gulf body, in its saw-toothed belly and in the lack of ourselves. -
The Evaluation of Wetland Restoration Potential Within the Sackville River Secondary Watershed
The Evaluation of Wetland Restoration Potential within the Sackville River Secondary Watershed Report Prepared by: McCallum Environmental Ltd. EVALUATION OF WETLAND RESTORATION POTENTIAL WITHIN THE SACKVILLE RIVER SECONDARY WATERSHED Proponents: Twin Brooks Development Ltd. Armco Capital Inc. Ramar Developments Ltd. Report Prepared by: McCallum Environmental Ltd. May 13, 2013 EXECUTIVE SUMMARY The purpose of this Evaluation of Wetland Restoration Potential (EWRP) study was to identify cost effective, practical and ecologically significant wetland restoration opportunities within the Sackville River Secondary Watershed, Nova Scotia. The EWRP is not a new study methodology in the North American context, but it is a relatively new methodology and study for Atlantic Canada. In Nova Scotia, the Department of Natural Resources owns and operates the Wetlands Inventory Database. This database is currently used to identify wetland habitat in Nova Scotia. However, it is commonly understood within industry and government that this database significantly underrepresents the quality and quantity of wetlands throughout the province of Nova Scotia. Therefore, EWRP first identified and evaluated a GIS tool, the potential wetland layer (PWL), to aid in the identification of potential wetland habitat. This PWL was created for the entire Sackville River Secondary Watershed. In addition to the PWL, a modeled stream layer that was developed by Mr. Raymond Jahncke of Dalhousie University, was also relied upon. It is crucial to note that the PWL is a desktop planning tool only and cannot replace field assessment and appropriate wetland delineation efforts. The PWL can be used to focus field efforts and begin to understand surface water systems across a property. -
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