DOCSLIB.ORG

Greenland & Wild Labrador 2014 Aboard the Sea Adventurer

Total Page：16

File Type：pdf, Size：1020Kb

Download full-text PDF Read full-text
Greenland & Wild Labrador 2014 Aboard the Sea Adventurer Greenland & Wild Labrador 2014 Aboard the Sea Adventurer Day 1 — Thursday September 11, 2014 "Traveler, there is no path, paths are made by walking." —Antonio Machado Kangerlussuaq From our charter plane you will catch your first glimpse of the magnificent Söndre Strömfjord, one of the longest fjords in the world. The fjord boasts a staggering 168 km of superb scenery. Kangerlussuaq, the town at the eastern end, means 'the big fjord.' Although the fjord crosses the Arctic Circle, like the oceans here, it does not freeze. Locals can thank ocean currents for this; they make this part of Greenland a centre for whaling and fishing year-round. The USA built an air base here in WWII due to the relatively mild weather and strategic location in relation to Europe. Although the military base closed in 1992, the strip is now Greenland's main international and domestic airport. The area is distinguished by fantastic nature and rich biodiversity. There is nowhere else in Greenland where the country’s interior may be so easily accessed. The landscape features enormous glacier formations, which have ploughed deep into the dramatic tundra. On the plain between the fjord and the inland ice you will find Greenland's biggest herds of musk ox, reindeer, arctic foxes, the highest concentration of peregrine falcons in Greenland, and more than 250 species of plants. 0500 check out from the Sheraton Gateway Hotel, proceed to Terminal 3 with your luggage to check-in counter #303 – 306 - - Check in is by surname - Group A-H 0530hrs / Group I-M 0600hrs / Group N-Z 0630hrs 0700 proceed through security to await your boarding call for Miami Air #611 0800 flight departs from Toronto 1400 expected arrival to Kangerlussuaq, Greenland, join coaches for our Kangerlussauq programme. 1630 transfer to Pier for our zodiac ride to our vessel MV Sea Adventurer Welcome aboard the MV Sea Adventurer, you will be met at reception and shown to your cabins, take a moment to check your luggage is in your cabin, if not please advise our reception staff. Then it’s your time to familiarize yourself with your cabin and throughout the ship, your home away from home for the voyage. Listen to announcements for the programme on board 1930 Dinner is served in the dining room - take a seat where ever you choose, your wait staff will take your order. For your onboard beverages Greenlandic Viking, Viking Explorer and Arctic Adventure wine packages are available Officers and Expedition Staff of M.V.Sea Adventurer Captain: Master Peter Gluschke Chief Officer: Donael Soto Chief Engineer: Marinko Hrabar Bartender: Eladio Bajan Purser: Willie Lirio Head Housekeeper: Winston Smart Maitre D’hotel: Narendra Seeram Chef: James Salmon Expedition Leader: Matt James Bradley-Swan Hotel Manager: Siegfried Schober Adventure Canada Host: Cedar Bradley-Swan Adventure Canada : Gay Peppin Culturalist: Maria Dicker Archaeologist/ Historian: Callum Thompson Archaeologist/ Historian: Jane Sproull Thompson Naturalist: Holly Hogan Author: Michael Crummey Artist / Culturalist: Pete Barrett Musician: Marshall Dane Culturalist/ Musician: Leander Baikie Photographer: Grant Stovel Artist: Rob Saley Expedition Team: Jason Edmunds Adventure Canada: Michael Strizic Inuit Art Specialist: Heather Beecroft Photographer/ Naturalist: Dennis Minty Geologist: Scott Schillereff Culturalist: Derrick Pottle Naturalist: Janet Bradshaw Musician: Daniel Payne On behalf of Captain Peter Gluschke, his Officers and Crew, and Adventure Canada we would like to warmly welcome you onboard the Sea Adventurer on our Greenland and Wild Labrador expedition. Greenland & Wild Labrador 2014 Aboard the Sea Adventurer Day 2 — Friday September 12, 2014 "No, no! The adventures first, explanations take such a dreadful time.” - Lewis Carroll, Alice's Adventures in Wonderland & Through the Looking-Glass Evighedsfjord & Kangaamiut Kangerlussuatsiaq Fjord (old spelling: Kangerdlugssuatsiaq, Danish: Evighedsfjorden) is a fjord in the Qeqqata municipality in western Greenland. Taking its source in the tidewater glaciers draining the Maniitsoq ice sheet, the fjord flows in a deep canyon through a mountainous, uninhabited region, emptying into Davis Strait near the settlement of Kangaamiut. Kangerlussuatsiaq Fjord is 75 km long and 700 m deep. The forbidding nature of the fjord surroundings preclude settlement for the majority of its length. Kangaamiut is the only settlement in the vicinity, located on a small island at the northern end of the fjord mouth. Kangaamiut had a population of 357 as of 2010, and has experienced a steady decline in population over a long period of time. In 1990, the population was 552, and in 2000 it was 481. Kangaamiut is located on an island off the coast of Davis Strait between the mouths of two long fjords. South of the island, the long and twisted Kangerlussuatsiaq Fjord empties into the sea, while immediately to the north, the Kangaamiut Kangerluarsuat Fjord flows into the sea between skerries. The mouth of the long Kangerlussuaq Fjord is located approximately 26 km north of the island. 0630 Early Bird Breakfast in the forward lounge 0700 Wake-up Call 0730 Breakfast is served in the dining room 0830 MANDATORY ZODIAC BREIFING and to discuss the plan for today 0930 Even Cabins passengers disembark for zodiac cruise at Evighedsfjord 0945 Odd Cabins passengers disembark for zodiac cruise at Evighedsfjord 1100 All aboard the Sea Adventurer 1130 From Snap Shots to Great Shots! Part one with Dennis Minty in the forward lounge 1230 Lunch is served in the dining room 1400 Odd Cabins disembark for Kangaamiut 1415 Even Cabins disembark for Kangaamiut 1730 Last zodiac departs Kangaamiut returning to the Sea Adventurer 1815 Join us in the forward lounge for Captains Welcome Cocktails and our Daily Briefing 1915 Dinner is served in the dining room 2100 Join us in the forward lounge to become aquatinted with the AC musicians! Inuktitut word of the day: Siku = Ice German saying of the day: Alles oder nichts = All or nothing Greenland & Wild Labrador 2014 Aboard the Sea Adventurer Day 3 — Saturday September 13, 2014 "I must down to the seas again, for the call of the running tide is a wild call and a clear call that may not be denied." —John Masefield Nuuk Nuuk is the seat of government for the Sermersooq municipality. It has a population of 15,469 (as of January 2010), making it one of the smallest capital cities in the world by population. Nuuk is located at approximately 64°10′00″N 51°44′00″W at the mouth of Nuup Kangerlua, some 10 kilometres from the shores of Labrador Sea on the southwestern coast of Greenland, and about 240 km south of the Arctic Circle. The area around Nuuk was first occupied by the ancient pre-Inuit, Paleo-Eskimo people of the Saqqaq culture as far back as 2200 BC, when they lived in the area around the now abandoned settlement of Qoornoq. For a long time it was occupied by the Dorset culture around the former settlement of Kangeq but they disappeared from the Nuuk district before AD 1000. Viking explorers in the 10th century inhabited the area; shortly thereafter, so did the Inuit peoples. Inuit and Norsemen lived with little interaction in this area from about AD 1000 until around AD 1500, when Norse settlement ended, probably due to changes in climate and vegetation. 0600 Early Bird Breakfast in the forward lounge 0630 Wake-up Call 0700 Breakfast is served in the dining room 0800 Even cabin passengers disembark Sea Adventurer for Nuuk 0815 Odd Cabin passengers disembark Sea Adventurer for Nuuk 1130 Shuttles commence from museum back to Sea Adventurer 1230 Last Shuttle departs museum to Sea Adventurer 1300 All aboard the Sea Adventurer as we depart fro Canada! 1300 Lunch is served in the dining room 1430 Join Scott in the forward lounge as he speaks on Bedrock Geology in Ancient Lands 1545 Identifying Seabirds at Sea with Holly Hogan 1700 Jane delivers her presentation: Keeping warm in the Cold in the forward lounge 1830 Join us for a daily recap in the forward lounge and a look towards tomorrow! 1915 Dinner is served in the dining room 2100 Join us in the forward lounge as we dance while Marshall Dane rocks! Inuktitut saying of the day: Kinauvit? = What is your name? German saying of the day: Darf ich Bitten = May I have this dance PLEASE SET YOUR CLOCKS BACK BY ONE HOUR WHEN YOU GO TO SLEEP Greenland & Wild Labrador 2014 Aboard the Sea Adventurer Day 4 — Saturday September 14, 2014 "Regions mountainous and wild, thinly inhabited, and little cultivated, make a great part of the earth, and he that has never seen them, must live unacquainted with much of the face of nature, and with one of the great scenes of human existence." —Samuel Johnson At Sea: Davis Strait Our presentation series will kick into full swing today as we steam across the Davis Strait towards Canada, and more adventure. Davis Strait is a wide, northerly arm of the Labrador Sea, separating Greenland from Baffin Island and containing some of the deepest water (as deep as 3360 m) in the Arctic. It is named for the English explorer John Davis, who explored the region from 1585-1587. Davis's explorations renewed awareness of Greenland among Europeans. Davis charted much of the region in his search for the Northwest Passage. By the 17th century, whaling had begin in Davis Strait, and by the peak of the industry (1820-1840) as many as a hundred vessels worked the Strait each year, taking as many as a thousand whales annually. Take advantage of a day aboard the Sea Adventurer to explore the nooks and crannies of our vessel, take in one of the many talks offered by our expert expedition staff. While out on deck, keep your eyes peeled for Minke and Orca whales, as well as a variety of other marine wildlife.
Load more

Recommended publications
  • The Concentration of in Situ 10Be in Fluvial Sediments As a Tool for Deciphering 6 My of Greenland Ice Sheet History from a Marine Sediment Core
    THE CONCENTRATION OF IN SITU 10BE IN FLUVIAL SEDIMENTS AS A TOOL FOR DECIPHERING 6 MY OF GREENLAND ICE SHEET HISTORY FROM A MARINE SEDIMENT CORE A Progress Report By Alice Heller Nelson To The Faculty of the Geology Department Of The University of Vermont 4th of October 2012 Accepted by the Faculty of the Geology Department, the University of Vermont, in partial fulfillment of the requirements for the degree of Master of Science specializing in Geology. The following members of the Thesis Committee have read and approved this document before it was circulated to the faculty: _________________________ Chair Jason D. Stockwell, Ph.D. _________________________ Advisor Paul R. Bierman, Ph.D. _________________________ Andrea Lini, Ph.D. Date Accepted: ________________ I. Introduction 1.1. Motivation My research involves measuring the concentration of in situ 10Be in glacio- fluvial sediments from Greenland and an adjacent ocean sediment core spanning the past 6 Myr (Figure 1). Knowing the concentration of 10Be in modern continental sediment samples will help me interpret the down core record, which may provide a new way of estimating timing of Greenland Ice Sheet (GIS) inception and inferring past ice extent and erosivity. Linking this ice sheet variability with records of past climate change may help to determine thresholds for ice loss and regrowth, which is an important step towards predicting how the ice sheet might respond to future climate change. 1.2. Project Goals The first component of my research is to measure the 10Be concentration in sediment sourced from different places on the Greenlandic landscape. Ice shields rock from cosmic rays, so I expect sediments sourced from glaciated versus ice-free terrain will contain different amounts of 10Be and that sediments from different source areas will mix as they are transported through the landscape.
    [Show full text]
  • Road Construction in Greenland – the Greenlandic Case
    THIS PROJECT IS BEING PART-FINANCED BY THE EUROPEAN UNION EUROPEAN REGIONAL DEVELOPMENT FUND ROAD CONSTRUCTION IN GREENLAND – THE GREENLANDIC CASE October 2007 Arne Villumsen Anders Stuhr Jørgensen Abdel Barten Janne Fritt-Rasmussen Laust Løgstrup Niels Brock Niels Hoedeman Ragnhildur Gunnarsdóttir Sara Borre Thomas Ingeman-Nielsen ROAD CONSTRUCTION IN GREENLAND – THE GREENLANDIC CASE October 2007 Arne Villumsen Anders Stuhr Jørgensen Abdel Barten Janne Fritt-Rasmussen Laust Løgstrup Niels Brock Niels Hoedeman Ragnhildur Gunnarsdóttir Sara Borre Thomas Ingeman-Nielsen Translation: J. Richard Wilson CONTENTS 1. GEOLOGY, NatURE AND CLIMate OF GREENLAND ........................... 4 1.1. GEOLOGY. 4 1.2. CLIMate . .5 1.3. Weather AND CLIMate IN AND AROUND GREENLAND . .5 1.4. Precipitation . .5 1.5. Weather- AND CLIMate REGIONS IN GREENLAND . .6 1.6. PERMAFROST. .9 1.7. Vegetation. .10 2. Relevant INFORMation FOR ROAD-BUILDING PROJECTS IN GREENLAND ........................................................................................... 11 3. EXISTING ROADS IN towns AND VILLAGES IN GREENLAND ......... 17 3.1. EXAMination OF EXISTING ROADS IN towns AND VILLAGES IN GREENLAND. 19 3.1.1. ROADS IN SISIMIUT town. .19 3.1.2. SISIMIUT Airport . 19 3.1.3. THE ROAD FROM KANGERLUSSSUAQ to THE INLAND ICE. 20 3.1.4. KANGERLUSSUAQ Airport. 21 3.2. STUDIES OF ROADS ELSEWHERE IN GREENLAND. .22 3.2.1. SOUTH GREENLAND . 23 3.2.2. ILLORSUIT. .27 4. THE SISIMIUT-KANGERLUSSUAQ ROAD ............................................ 32 4.1. GEOLOGICAL AND GEOGRAPHICAL overview. .32 4.2. SUitable Materials FOR ROAD CONSTRUCTION AND PERMAFROST. .35 4.3. GEOLOGICAL MODEL FOR THE AREA. 39 4.4. SUMMARY. .55 4.5. ENVIRONMental AND conservation ASPECTS. .55 4.6. ROUTE PROPOSAL – GENERAL ASPECTS.
    [Show full text]
  • AMERICAN MUSEUM NOVITATES Published by Number 895 the AMERICAN MUSEUM of NATURAL HISTORY Dec
    AMERICAN MUSEUM NOVITATES Published by Number 895 THE AMERICAN MUSEUM OF NATURAL HISTORY Dec. 31 1936 New York City THE NEARCTIC ATYPIDAE By W. J. GERTSCH The curious spiders now comprising the Atypidae were set apart many years ago by various authors as representing a group which, though obviously closely related to the other mygalomorph species, was worthy of separation from them in some way, either as a genus, a sub- family, or a family. The genus Atypus dates from 1804, when Latreille used the name for the first time in a generic sense. Aranea subterranea Roemer, now placed as a synonym of Atypus piceus (Sulzer), was desig- nated as the genotype by this same author in 1810. Ausserer in his 'Beitrage zur Kenntniss der Arachniden-Familie der Territelariae' recognized a subfamily Atypinae, which name had been used pro- visionally by Thorell in 1869-1870, and included three generic cate- gories, Calommata Lucas, its synonym Pelecodon Doleschal, and Atypus Latreille. This author placed two of the American species in Atypus but erected the new genus Madognatha for Sphodros abbotii Walckenaer, assigning it to the subfamily Theraphosinae. The family name, Atypidae, was proposed by P. Bertkau in 1878 and was based on the characters presented in the German species of Atypus. A little later Thorell (1889-1890) divided his Territelariae into five families and for some reason substituted the name Calommatoidae for the Atypidae of Bertkau. In the 'Historie Naturelle des Araginees' Simon restored the name Atypidae and considerably enlarged the limits of the family by including twenty-four species representing six genera, and placed them in three subfamilies, the Brachybothrinae, Hexurinae, and Atypinae.
    [Show full text]
  • Large Surface Meltwater Discharge from the Kangerlussuaq Sector Of
    The Cryosphere, 6, 199–209, 2012 www.the-cryosphere.net/6/199/2012/ The Cryosphere doi:10.5194/tc-6-199-2012 © Author(s) 2012. CC Attribution 3.0 License. Large surface meltwater discharge from the Kangerlussuaq sector of the Greenland ice sheet during the record-warm year 2010 explained by detailed energy balance observations D. van As1, A. L. Hubbard2, B. Hasholt3, A. B. Mikkelsen3, M. R. van den Broeke4, and R. S. Fausto1 1Geological Survey of Denmark and Greenland, Øster Voldgade 10, 1350 Copenhagen K, Denmark 2Institute of Geography and Earth Sciences, Aberystwyth University, Llandinam Building, Penglais Campus, Aberystwyth, SY23 3DB, Wales 3Department of Geography and Geology, Øster Voldgade 10, 1350 Copenhagen K, Denmark 4Institute for Marine and Atmospheric Research, Utrecht University, Princetonplein 5, 3584 CC Utrecht, The Netherlands Correspondence to: D. van As ([email protected]) Received: 15 August 2011 – Published in The Cryosphere Discuss.: 6 September 2011 Revised: 28 December 2011 – Accepted: 3 January 2012 – Published: 13 February 2012 Abstract. This study uses data from six on-ice weather sta- 1 Introduction tions, calibrated MODIS-derived albedo and proglacial river gauging measurements to drive and validate an energy bal- Greenland stores nearly three million cubic kilometres of ice, ance model. We aim to quantify the record-setting positive a large potential contribution to sea level rise. In recent years, temperature anomaly in 2010 and its effect on mass bal- increasingly large areas of the ice sheet have been losing ance and runoff from the Kangerlussuaq sector of the Green- mass, as determined from its satellite-derived gravity field ◦ land ice sheet.
    [Show full text]
  • Vejprojekt Mellem Kangerlussuaq Og Sisimiut
    Vej mellem Sisimiut og Kangerlussuaq Konsekvensanalyse af fordele og ulemper Sisimiut Kommune 1 Vej mellem Sisimiut og Kangerlussuaq Konsekvensanalyse af fordele og ulemper Udarbejdet af: Laust Løgstrup Naja Joelsen Anette G. Lings Inunnguaq Lyberth Peter Evaldsen Rasmus Frederiksen Klaus Georg Hansen Morten H. Johansen Finn E. Petterson Larseraq Skifte Sisimiut Kommune Marts 2003 2 Vej mellem Sisimiut og Kangerlussuaq - konsekvensanalyse af fordel og ulemper © Sisimiut Kommune Sisimiut marts 2003 Printet hos Sisimiut Kommune Printede eksemplarer af rapporten kan rekvireres ved henvendelse til: Sisimiut Kommune Postboks 1014 DK-3911 Sisimiut Grønland E-mail: [email protected] Rapporten kan også hentes som PDF-fil på adressen: http://www.sisimiut.gl/vej Redaktionen er afsluttet den 21. marts 2003. Mekanisk, fotografisk eller anden gengivelse af denne rapport eller dele af den er tilladt med angivelse af kilde. Fotoet på forsiden er fra Haines i Yukon i Canada og er venligst stillet til rådighed af Yukons Regering. 3 Indholdsfortegnelse INDHOLDSFORTEGNELSE.................................................................................................3 SAMMENDRAG ......................................................................................................................5 INDLEDNING ..........................................................................................................................9 BAGGRUND...............................................................................................................................9
    [Show full text]
  • GREENLAND Summer and Winter Adventures
    GREENLAND summer and winter adventures Greenland summer and winter adventures 1 Greenland with Albatros Travel With a strong foothold in Kangerlussuaq, we can provide your clients with a seamless experience of Greenland. Three Table of decades ago, we were one of the first travel operators to venture into the arctic wilderness of Greenland. Today, we CONTENTS have cemented our presence there in the form of a local office, restaurant, gift shop and two hostels. 2 INTRODUCTION 4-5 YOUR GATEWAY TO GREEENLAND Find out more about our Greenland operations on page 4. 8-9 SHIP: OCEAN DIAMOND Why Albatros 6-7 SUMMER TOURS Greenland holds a special place in our hearts here at Albatros Travel. With headquarters 8-9 GREENLAND’S MAGICAL MIDNIGHT SUN in Copenhagen, Denmark, our connection to this vast continent is like that of all Danes. 10-11 MAGNIFICENT GREENLAND The joint history has been murky and at times dark. However, we are determined to show - ICE SHEET AND ICEBERGS guests from abroad how incredibly beautiful and untouched Greenland is. 12-13 SUMMER IN ICELAND AND ILULISSAT We cherish the wide, open spaces, the long, dark winters only brightened by the sparkling 14-15 TREASURES OF SOUTH GREENLAND snow, breathtaking northern lights (the aurora borealis), the short, and surprisingly green summers lit by the midnight sun, the seemingly endless icescapes and the warmth of the 16-17 WINTER TOURS Greenlandic people. Yes, the list is long and we could go on. 18-19 WINTER WONDERLAND IN GREENLAND We don’t just know Greenland’s history, the names of its birds, wildlife and its nature.
    [Show full text]
  • Location Privacy Without Mutual Trust: the Spatial Bloom Filter
    CORE Metadata, citation and similar papers at core.ac.uk Provided by Bournemouth University Research Online Location privacy without mutual trust: the Spatial Bloom Filter a, b a Luca Calderoni ∗, Paolo Palmieri , Dario Maio aDepartment of Computer Science and Engineering, University of Bologna, Cesena, FC, 47521 Italy bBournemouth University, Poole, Dorset, BH12 5BB, UK Abstract Location-aware applications are one of the biggest innovations brought by the smartphone era, and are effectively changing our everyday lives. But we are only starting to grasp the privacy risks associated with constant tracking of our whereabouts. In order to continue using location-based services in the future without compromising our privacy and security, we need new, privacy-friendly applications and protocols. In this paper, we propose a new compact data structure based on Bloom filters, designed to store location information. The Spatial Bloom Filter (SBF), as we call it, is designed with privacy in mind, and we prove it by presenting two private positioning protocols based on the new primitive. The protocols keep the user’s exact position private, but allow the provider of the service to learn when the user is close to specific points of interest, or inside predefined areas. At the same time, the points and areas of interest remain oblivious to the user. The two proposed protocols are aimed at different scenarios: a two-party setting, in which communication happens directly between the user and the service provider, and a three-party setting, in which the service provider outsources to a third party the communication with the user. A detailed evaluation of the efficiency and security of our solution shows that privacy can be achieved with minimal computational and communication overhead.
    [Show full text]
  • Next Generation Space Defense May 2021
    Next Generation Space Defense MilsatMagazineMilsatMagazine May 2021 Cover image: United Launch Alliance’s Delta IV Heavy rocket carrying the NROL-82 mission for the National Reconnaissance Office lifts off from Space Launch Complex-6 at Vandenberg Air Force Base in California. Image Source: United Launch Alliance Beyond Secure Satcoms Publishing OPeratiOns disPatChes Features Eutelsat + OneWeb .................................................. 4 How SATCOM Vastly Improves .............................. 12 Silvano Payne, Publisher + Executive Writer Small UAV Flexibility Simon Payne, Chief Technical Officer Author: Get SAT Hartley G. Lesser, Editorial Director ULA + NRO ............................................................... 6 Pattie Lesser, Executive Editor Donald McGee, Production Manager USSF/SMC + Raytheon I&S ...................................... 8 Teresa Sanderson, Operations Director Sean Payne, Business Development Manager Lockheed Martin ....................................................... 8 Dan Makinster, Technical Advisor High Availability Maritime SATCOM....................... 18 Starts On The Ship Space Flight Laboratory ......................................... 10 Author: Dr. Rowan Gilmore, EM Solutions seniOr COlumnists Virgin Orbit ............................................................ 11 and COntributOrs Hughes + OneWeb ................................................. 15 Delivering Mission-Critical Connectivity with ........ 28 Chris Forrester, Broadgate Publications Reliability and Resilience Loft Orbital
    [Show full text]
  • Éditeur Officiel Du Québec Updated to August 1 2016 This Document Has Official Status
    0 0 8 1 © Éditeur officiel du Québec Updated to August 1 2016 This document has official status. chapter R-20, r. 6.1 Regulation respecting the hiring and mobility of employees in the construction industry L A Act respecting labour relations, vocational training and workforce management in the construction industry B O(chapter R-20, s. 123.1, subpar. 13) RU 1O-R 2D.R eC0E TABLE OF CONTENTS c.L e1A m9 DIVISION I T DEFINITIONS.................................................................................................... 1 b4I e6O DIVISION II r-N DIVISION III 38S 02— DIVISION IV ,;C SO DIVISION V 1.N HIRING............................................................................................................... 35 8QS DIVISION VI 9.T GENERAL PROVISIONS.................................................................................. 40 91R 9U 9C 3T ,I cO .N 6— 1H ,I sR .I 7N 2G .A N D M O B I L I T Y Updated to 0August 01 2016 © Éditeur officiel8 du1 Québec R-20, r. 6.1 / 1 of 23 LABOUR RELATIONS — CONSTRUCTION — HIRING AND MOBILITY DIVISION I DEFINITIONS 1. In this Regulation, unless the context requires otherwise, “apprentice” means a person holding an apprentice competency certificate issued under the Regulation respecting the issuance of competency certificates (chapter R-20, r. 5); “remote site” means a site inaccessible by a passable road connected to the roads network of the Province of Québec and the James Bay region; “graduate” means a person with a secondary school diploma granted for one of the construction trades and issued by an institution recognized by the Ministère de l’Éducation, du Loisir et du Sport; “remote area” means an area inaccessible by a passable road connected to the roads network of the Province of Québec, and an island situated along the St.
    [Show full text]
  • Validation of Globsnow-2 Snow Water Equivalent Over Eastern Canada
    1 Validation of GlobSnow-2 snow water equivalent over 2 Eastern Canada 3 Fanny Larue1,2,3, Alain Royer1,2, Danielle De Sève3, Alexandre Langlois1,2, Alexandre 4 Roy1,2 and Ludovic Brucker4,5 5 1 Centre d’Applications et de Recherches en Télédétection, Université de Sherbrooke, 6 Sherbrooke, Québec, Canada 7 2 Centre for Northern Studies, Québec, Canada 8 3 IREQ Hydro-Québec, Varenne, Québec, Canada 9 4 NASA GSFC, Cryospheric Sciences Laboratory, Greenbelt, MD 20771, USA 10 5 Universities Space Research Association, Goddard Earth Sciences Technology and Research 11 Studies and Investigations, Columbia, MD 21044, USA 12 13 * Correspondance: Fanny Larue, CARTEL, Département de Géomatique Appliquée, 14 Université de Sherbrooke, 2500 Blvd. de l’Université, Sherbrooke, QC J1K 2R1, Canada. 15 E-mail address: [email protected] 16 17 Abstract: In Québec, Eastern Canada, snowmelt runoff contributes more than 30% of 18 the annual energy reserve for hydroelectricity production, and uncertainties in annual 19 maximum snow water equivalent (SWE) over the region are one of the main 20 constraints for improved hydrological forecasting. Current satellite-based methods for 21 mapping SWE over Québec's main hydropower basins do not meet Hydro-Québec 22 operational requirements for SWE accuracies with less than 15% error. This paper 23 assesses the accuracy of the GlobSnow-2 (GS-2) SWE product, which combines 24 microwave satellite data and in situ measurements, for hydrological applications in 25 Québec. GS-2 SWE values for a 30-year period (1980 to 2009) were compared with 26 space- and time-matched values from a comprehensive dataset of in situ SWE 27 measurements (a total of 38 990 observations in Eastern Canada).
    [Show full text]
  • Why Should We Care About Greenland Watersheds? Reactions, Runoff, and Rising Sea Level
    Why should we care about Greenland watersheds? Reactions, runoff, and rising sea level Jon Martin Ellen Martin Cecilia Scribner Kelly Deuerling Daniel Collazo Adam Marshall Greenland Watersheds Subglacial Proglacial Deglacial Subglacial Proglacial Deglacial Water Melt water Modified from system discharged Water from annual Anderson, 2007, under the from the ice precipitation and Ann. Rev. Earth permafrost melt ice sheet Planet Sci Significance: Watershed Variations ~20ky Now Last Glacial Maximum Mostly deglacial All sub- & pro-glacial Much weathered material Much fresh material Implication 1: Sea level rise • Spectacular events: – (MWP1A) 14.5 – 14.0 ka BP > 40 mm/yr – Reflect rapid collapse of continental ice sheets • Change in the material fluxes: – To ocean: isotopes & nutrients (?) – With atmosphere: CO2 Forward in time Lambeck et al., 2014, PNAS Implication 2: Runoff (and fluxes) • Systematic shifts in Pb isotopes in North Atlantic sediments: Sea level – Rapid increase during rapid SL rise Orphan knoll – Gradual drift down following SL rise Laurentian Fan • Reflect changes in Blake Ridge runoff composition (reactions) Lambeck et al., 2014, PNAS; Gutjahr et al., 2009, EPSL; Kurzweil et al., 2010, EPSL; Crocket et al., 2012 Implications 3: Reactions Large D values • Offset between whole rock and leached material Small D – Represent weathering values products • Offset increases with younger material Large D • Causes: values – Change in minerals being weathered (Sr) – Availability of radiogenic Small D isotopes in damaged values crystal lattices (Pb) Upper: Harlavan et al., 1998, GCA; Lower: Blum and Erel, 1997, GCA Hypotheses • Hypothesis 1: • Weathering Laurentian Fan, North Atlantic extent/products should vary across watershed types • Hypothesis 2: • Solutes in addition to Pb should vary with Kurzweil et al.
    [Show full text]
  • A Major Collapse of Kangerlussuaq Glacier's Ice Tongue Between 1932 and 1933 in East Greenland
    A Major Collapse of Kangerlussuaq Glacier's Ice Tongue Between 1932 and 1933 in East Greenland Vermassen, Flor; Bjørk, Anders A.; Sicre, Marie Alexandrine; Jaeger, John M.; Wangner, David J.; Kjeldsen, Kristian K.; Siggaard-Andersen, Marie Louise; Klein, Vincent; Mouginot, Jeremie; Kjær, Kurt H.; Andresen, Camilla S. Published in: Geophysical Research Letters DOI: 10.1029/2019GL085954 Publication date: 2020 Document version Publisher's PDF, also known as Version of record Document license: CC BY Citation for published version (APA): Vermassen, F., Bjørk, A. A., Sicre, M. A., Jaeger, J. M., Wangner, D. J., Kjeldsen, K. K., Siggaard-Andersen, M. L., Klein, V., Mouginot, J., Kjær, K. H., & Andresen, C. S. (2020). A Major Collapse of Kangerlussuaq Glacier's Ice Tongue Between 1932 and 1933 in East Greenland. Geophysical Research Letters, 47(4), [e2019GL085954]. https://doi.org/10.1029/2019GL085954 Download date: 04. okt.. 2021 RESEARCH LETTER A Major Collapse of Kangerlussuaq Glacier's Ice Tongue 10.1029/2019GL085954 Between 1932 and 1933 in East Greenland Key Points: Flor Vermassen1,2 , Anders A. Bjørk2 , Marie‐Alexandrine Sicre3, John M. Jaeger4, • Historical evidence reveals a major 1,2 1 2 collapse of Kangerlussuaq Glacier's David J. Wangner , Kristian K. Kjeldsen , Marie‐Louise Siggaard‐Andersen , ice tongue between 1932 and 1933 Vincent Klein3, Jeremie Mouginot5,6 , Kurt H. Kjær2, and Camilla S. Andresen1 • The collapse was likely triggered by increasing air and ocean 1Department of Glaciology and Climate, GEUS, Copenhagen, Denmark,
    [Show full text]