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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. -
Provincial Solidarities: a History of the New Brunswick Federation of Labour
provincial solidarities Working Canadians: Books from the cclh Series editors: Alvin Finkel and Greg Kealey The Canadian Committee on Labour History is Canada’s organization of historians and other scholars interested in the study of the lives and struggles of working people throughout Canada’s past. Since 1976, the cclh has published Labour / Le Travail, Canada’s pre-eminent scholarly journal of labour studies. It also publishes books, now in conjunction with AU Press, that focus on the history of Canada’s working people and their organizations. The emphasis in this series is on materials that are accessible to labour audiences as well as university audiences rather than simply on scholarly studies in the labour area. This includes documentary collections, oral histories, autobiographies, biographies, and provincial and local labour movement histories with a popular bent. series titles Champagne and Meatballs: Adventures of a Canadian Communist Bert Whyte, edited and with an introduction by Larry Hannant Working People in Alberta: A History Alvin Finkel, with contributions by Jason Foster, Winston Gereluk, Jennifer Kelly and Dan Cui, James Muir, Joan Schiebelbein, Jim Selby, and Eric Strikwerda Union Power: Solidarity and Struggle in Niagara Carmela Patrias and Larry Savage The Wages of Relief: Cities and the Unemployed in Prairie Canada, 1929–39 Eric Strikwerda Provincial Solidarities: A History of the New Brunswick Federation of Labour / Solidarités provinciales: Histoire de la Fédération des travailleurs et travailleuses du Nouveau-Brunswick David Frank A History of the New Brunswick Federation of Labour david fra nk canadian committee on labour history Copyright © 2013 David Frank Published by AU Press, Athabasca University 1200, 10011 – 109 Street, Edmonton, ab t5j 3s8 isbn 978-1-927356-23-4 (print) 978-1-927356-24-1 (pdf) 978-1-927356-25-8 (epub) A volume in Working Canadians: Books from the cclh issn 1925-1831 (print) 1925-184x (digital) Cover and interior design by Natalie Olsen, Kisscut Design. -
Prof Michael Fasham Collection
National Oceanographic Library - Archive Prof Michael Fasham FRS, Collection Mike Fasham joined the National Institute of Oceanography in 1968 and, with Jim Crease, developed one of the first shipboard computer systems in the world. He also began cooperating with Martin Angel, to use multivariate statistical techniques to analyse the zoogeographic distribution of zooplankton. This was a major achievement in a field which was largely descriptive at the time, and in 1973 he joined the Marine Biology department, where he brought his strong mathematical skills to bear on a range of topics. In the late 70s and early 80s, Mike worked on the centuries old question of what produces spatial variability, or “patchiness”, in plankton, using both theoretical and observational approaches. He added an in situ fluorometer to the SeaSoar undulator to map the small-scale distribution of phytoplankton. Between 1970 and 1980, he carried out theoretical and observational studies of temporal and spatial distributions of plankton, and developed models of the ocean carbon and nitrogen cycles. He also had a strong interest in the role of the oceans in climate change. His classic paper ‘A nitrogen-based model of plankton dynamics in the oceanic mixed layer’ (1990) has been cited more than 500 times. The Fasham-Ducklow-McKelvie model, as it became known, was subsequently embedded in the first three-dimensional ecosystem model of the Atlantic developed at Princeton University. Mike Fasham became Head of the Biological Modelling Group in the George Deacon Division of the Southampton Oceanography Centre (SOC), which was established in 1995. From 1998 to 2000, he also served as chairman of the international committee of the Joint Global Ocean Flux Study (JGOFS), which was aimed at understanding the fluxes of carbon and associated nutrients in the ocean Mike Fasham played a key role in the development of the international Joint Global Ocean Flux Study (JGOFS), serving on the National and International Committees and ultimately as chair of the International Committee from 1998 to 2000. -
Atlantic Zone Based on Satellite Data, and (3) Egg and Larval Distributions of Cod and Haddock from Cape Hatteras to the Laurentian Channel
Fisheries and Oceans Pêches et Océans Science Sciences C S A S S C É S Canadian Stock Assessment Secretariat Secrétariat canadien pour l’évaluation des stocks Proceedings Series 2000/17 Série des compte rendus 2000/17 Final Report of the 2000 Annual Meeting of the Fisheries Oceanography Committee Including the Report of the Workshop on the Cod Recruitment Dilemma February 22-25, 2000 Northwest Atlantic Fisheries Center St. John’s, Newfoundland 1D.P. Swain, Chairperson (FOC) 2M. Castonguay, Chairperson (Cod Recruitment Workshop) 1Fisheries and Oceans Canada 343 Ave Université Ave Moncton, New-Brunswick E1C 9B6 2Fisheries and Oceans Canada Institut Maurice Lamontagne 850 Route de la Mer, C.P. 1000 G5H 3Z4 September 2000 ii Executive Summary of the 2000 FOC Annual Meeting The Fisheries Oceanography Committee (FOC) of the Department of Fisheries and Oceans (DFO) met in St. John’s, Newfoundland at the Northwest Atlantic Fisheries Center on 22-25 February 2000. The Committee reviewed environmental conditions in the Northwest Atlantic during 1999, convened a workshop on the Cod Recruitment Dilemma, reviewed additional papers on physical and biological oceanography and on changes in cod diets, and conducted its annual business meeting. 1. Physical Environment in 1999: Eight papers were reviewed on the meteorological and physical oceanographic conditions in 1999. Air temperature warmed relative to 1998 throughout most of the northwest Atlantic, reaching record high values in the Gulf of St. Lawrence, on the Scotian Shelf and over eastern Newfoundland. Sea ice coverage and duration were below average in most areas. Water temperatures from southern Labrador to the Grand Bank and off southern Newfoundland were generally above normal values.This was reflected in below-average volumes of the cold intermediate layer (CIL) and warmer- than-average bottom waters off Newfoundland, especially on the Grand Bank where bottom temperatures were 1-3°C above average. -
Geology of the Island of Grand Manan, New Brunswick: Precambrian to Early Cambrian and Triassic Formations
GEOLOGICAL ASSOCIATION OF CANADA / MINERALOGICAL ASSOCIATION OF CANADA JOINT ANNUAL MEETING 2014 UNIVERSITY OF NEW BRUNSWICK, FREDERICTON, NEW BRUNSWICK, CANADA FIELD TRIP B3 GEOLOGY OF THE ISLAND OF GRAND MANAN, NEW BRUNSWICK: PRECAMBRIAN TO EARLY CAMBRIAN AND TRIASSIC FORMATIONS MAY 23–25, 2014 J. Gregory McHone 1 and Leslie R. Fyff e 2 1 9 Dexter Lane, Grand Manan, New Brunswick, E5G 3A6 2 Geological Surveys Branch, New Brunswick Department of Energy and Mines, PO Box 6000, Fredericton, New Brunswick, E3B 5H1 i TABLE OF CONTENTS List of Figures and Tables..............................................................................................................i Safety............................................................................................................................................ 1 Itinerary ......................................................................................................................................... 2 Part 1: Geology of the Island of Grand Manan......................................................................... 3 Introduction ................................................................................................................................... 3 Precambrian Terranes of Southern New Brunswick ..................................................................... 3 Caledonia Terrane ............................................................................................................. 7 Brookville Terrane ............................................................................................................ -
Grand Manan Channel – Southern Part NOAA Chart 13392
BookletChart™ Grand Manan Channel – Southern Part NOAA Chart 13392 A reduced-scale NOAA nautical chart for small boaters When possible, use the full-size NOAA chart for navigation. Published by the 33-foot unmarked rocky patch known as Flowers Rock, 3.9 miles west- northwestward of Machias Seal Island, the channel is free and has a National Oceanic and Atmospheric Administration good depth of water. The tidal current velocity is about 2.5 knots and National Ocean Service follows the general direction of the channel. Daily predictions are given Office of Coast Survey in the Tidal Current Tables under Bay of Fundy Entrance. Off West Quoddy Head, the currents set in and out of Quoddy Narrows, forming www.NauticalCharts.NOAA.gov strong rips. Sailing vessels should not approach West Quoddy Head too 888-990-NOAA closely with a light wind. North Atlantic Right Whales.–The Bay of Fundy is a feeding and nursery What are Nautical Charts? area for endangered North Atlantic right whales (peak season: July through October) and includes the Grand Manan Basin, a whale Nautical charts are a fundamental tool of marine navigation. They show conservation area designated by the Government of Canada. (See North water depths, obstructions, buoys, other aids to navigation, and much Atlantic Right Whales, chapter 3, for more information on right whales more. The information is shown in a way that promotes safe and and recommended measures to avoid collisions with whales.) efficient navigation. Chart carriage is mandatory on the commercial Southwest Head, the southern extremity of Grand Manan Island, is a ships that carry America’s commerce. -
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, -
Real Property Issues in the Marine Aquaculture Industry in New Brunswick
REAL PROPERTY ISSUES IN THE MARINE AQUACULTURE INDUSTRY IN NEW BRUNSWICK SUE NICHOLS IAN EDWARDS JIM DOBBIN KATALIN KOMJATHY SUE HANHAM October 2001 TECHNICAL REPORT NO. 208217 REAL PROPERTY ISSUES IN THE MARINE AQUACULTURE INDUSTRY IN NEW BRUNSWICK Sue Nichols Ian Edwards Jim Dobbin Katalin Komjathy Sue Hanham Department of Geodesy and Geomatics Engineering University ofNew Brunswick P.O. Box 4400 Fredericton, N.B. Canada E3B 5A3 October 2001 PREFACE In order to make our extensive series of technical reports more readily available, we have scanned the old master copies and produced electronic versions in Portable Document Format. The quality of the images varies depending on the quality of the originals. The images have not been converted to searchable text. PREFACE This report was prepared under contract for the New Brunswick Department of Fisheries and Aquaculture. The research was carried out in 1997 at the University of New Brunswick, Fredericton, Canada, under the leadership of Professor Sue Nichols. As with any copyrighted material, permission to reprint or quote extensively from this report must be received from the authors. The citation to this work should appear as follows: Nichols, S., I. Edwards, J. Dobbin, K. Komjathy, and S. Hanham (2001). Real Property Issues in the Marine Aquaculture Industry in New Brunswick. Final contract report for the New Brunswick Department of Fisheries and Aquaculture, by the Geographical Engineering Laboratory, Department of Geodesy and Geomatics Engineering Technical Report No. 208, University of New Brunswick, Fredericton, New Brunswick, Canada, 102 pp. Real Property Issues in the Marine Aquaculture Industry in New Brunswick Acknowledgements The authors would like to thank for the Department of Fisheries and Aquaculture for recognising the need for this research and providing the funds. -
Crater Ice Deposits Near the South Pole of Mars Owen William Westbrook
Crater Ice Deposits Near the South Pole of Mars by Owen William Westbrook Submitted to the Department of Earth, Atmospheric, and Planetary Sciences in partial fulfillment of the requirements for the degree of Master of Science in Earth and Planetary Sciences at the MASSACHUSETTS INSTITUTE OF TECHNOLOGY June 2009 © Massachusetts Institute of Technology 2009. All rights reserved. A uth or ........................................ Department of Earth, Atmospheric, and Planetary Sciences May 22, 2009 Certified by . Maria T. Zuber E. A. Griswold Professor of Geophysics Thesis Supervisor 6- Accepted by.... ...... ..... ........................................... Daniel Rothman Professor of Geophysics Department of Earth, Atmospheric and Planetary Sciences MASSACHUSETTS INSTWITE OF TECHNOLOGY JUL 2 0 2009 ARCHIES LIBRARIES Crater Ice Deposits Near the South Pole of Mars by Owen William Westbrook Submitted to the Department of Earth, Atmospheric, and Planetary Sciences on May 22, 2009, in partial fulfillment of the requirements for the degree of Master of Science in Earth and Planetary Sciences Abstract Layered deposits atop both Martian poles are thought to preserve a record of past climatic conditions in up to three km of water ice and dust. Just beyond the extent of these south polar layered deposits (SPLD), dozens of impact craters contain large mounds of fill material with distinct similarities to the main layered deposits. Previously identified as outliers of the main SPLD, these deposits could offer clues to the climatic history of the Martian south polar region. We extend previous studies of these features by cataloging all crater deposits found near the south pole and quantifying the physical parameters of both the deposits and their host craters. -
CHAPTER 6 Thermal-Hydraulic Design
1 CHAPTER 6 Thermal-Hydraulic Design Prepared by Dr. Nikola K. Popov Summary This chapter covers the thermal-hydraulic design of nuclear power plants with a focus on the primary and secondary sides of the nuclear steam supply system. This chapter covers the following topics: evolution of the reactor thermal-hydraulic system; key design requirements for the heat transport system; thermal-hydraulic design principles and margins; design details of the primary and secondary heat transport systems; fundamentals of two-phase flow; fundamentals of heat transfer and fluid flow in the reactor heat transport system; other related topics. ©UNENE, all rights reserved. For educational use only, no assumed liability. Thermal-Hydraulic Design – December 2015 2 The Essential CANDU Table of Contents 1 Introduction........................................................................................................................... 10 1.1 Overview....................................................................................................................... 10 1.2 Learning outcomes........................................................................................................ 12 1.3 Summary of relationship to other chapters ................................................................... 12 1.4 Thermal-hydraulic design ............................................................................................. 12 2 Reactor Types ...................................................................................................................... -
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. -
Fluid Escape Structures As Possible Indicators of Past Gas Hydrate
DOI: 10.1590/2317‑4889201720160090 ARTICLE Fluid escape structures as possible indicators of past gas hydrate dissociation during the deposition of the Barremian sediments in the Recôncavo Basin, NE, Brazil Estruturas de escape de fluidos como possíveis indicadoras de uma paleo‑dissociação de hidratos de gás durante a deposição de sedimentos do Barremiano na Bacia do Recôncavo, NE, Brasil Antonio Fernando Menezes Freire1*, Carlson de Matos Maia Leite2, Flávio Miranda de Oliveira2, Márcio Ferreira Guimarães2, Paulo da Silva Milhomem2, Raphael Pietzsch3, Roberto Salvador Francisco d’Ávila4 ABSTRACT: Empty elliptical vesicles are observed in outcrops RESUMO: Vesículas elípticas ocas são observadas em afloramentos de areni- of Barremian very fine clayey sandstone to siltstone lacustrine tos argilosos muito finos e siltitos lacustrinos do Membro Pitanga da Formação slurry deposits of the Pitanga Member (Maracangalha Forma‑ Maracangalha, expostos na Ilha de Maré, sudeste da Bacia do Recôncavo, Es- tion), exposed in the Maré Island, Southern Recôncavo Basin, tado da Bahia, Brasil. Essas rochas foram depositadas em condições subaquo- Brazil. These sedimentary features have been traditionally in‑ sas e são consideradas depósitos gravitacionais do tipo slurry. Essas feições têm terpreted as water escape structures triggered by the diapirism sido tradicionalmente interpretadas como sendo estruturas de escape de água, of the underlying shales of the Candeias Formation. This work resultado da ação do diapismo de folhelhos sotopostos da Formação Candeias. proposes that vesicles were generated during massive gas hydrate Este trabalho propõe que as vesículas foram geradas durante uma intensa dis- dissociation as a result of tectonic activity in a paleolake system. sociação de hidratos de gás em resposta à atividade tectônica existente naquele Tectonic uplift would have triggered both the reduction of the sistema lacustre.