2006 Expedition Report

Total Page:16

File Type:pdf, Size:1020Kb

2006 Expedition Report 2006 Expedition Report CCGS Amundsen CCGS Pierre Radisson LEG 1 BaySys/ArcticNet ArcticNet Hudson Bay Baffin Bay and Canadian Arctic Archipelago LEG 2A ArcticNet Amundsen Gulf, Beaufort Sea and Canadian Arctic Archipelago LEG 2B ArcticNet Labrador fjords ArcticNet - Amundsen Science Program Université Laval Pavillon Alexandre-Vachon, room 4081 1045, avenue de la Médecine Québec, QC, G1V 0A6 CANADA www.amundsen.ulaval.ca www.arcticnet.ulaval.ca Anissa Merzouk ArcticNet Expedition Report Editor [email protected] Keith Levesque ArcticNet Marine Research Manager [email protected] Cover page photo credit Martin Fortier / ArcticNet Table of Content TABLE OF CONTENT II LIST OF FIGURES V LIST OF TABLES IX 2006 EXPEDITION REPORT 1 PART I – OVERVIEW AND SYNOPSIS OF OPERATIONS 2 1 OVERVIEW OF THE 2006 ARCTICNET EXPEDITION 2 1.1 Introduction 2 1.2 Regional settings 2 1.3 2006 CCGS Amundsen Expedition Plan 12 1.4 2006 CCGS Pierre Radisson Expedition Plan 13 2 LEG 1 22 AUGUST TO 28 SEPTEMBER 2006 BAFFIN BAY AND CANADIAN ARCTIC ARCHIPELAGO 14 2.1 Introduction and objectives 14 2.2 Synopsis of operations 16 2.3 Chief Scientist’s comments 19 3 LEG 2A 28 SEPTEMBER TO 29 OCTOBER 2006 AMUNDSEN GULF, BEAUFORT SEA AND CANADIAN ARCTIC ARCHIPELAGO 21 3.1 Introduction and objectives 21 3.2 Synopsis of operations 23 3.3 Chief Scientist’s comments 26 4 LEG 2B 29 OCTOBER TO 9 NOVEMBER 2006 LABRADOR FJORDS 27 4.1 Introduction and objectives 27 4.2 Synopsis of operations 29 4.3 Chief Scientist’s comments 31 5 BAYSYS 12 SEPTEMBER TO 24 SEPTEMBER 2006 HUDSON BAY 32 5.1 Introduction and objectives 32 5.2 Synopsis of operations 33 5.3 Chief Scientist’s comments 33 PART II – PROJECT REPORTS 34 1 METEOROLOGICAL, OCEANOGRAPHIC AND NAVIGATION DATA – LEGS 1, 2A AND 2B 34 1.1 Introduction 34 1.2 Description of systems and available data 34 ii 2 SURFACE METEOROLOGY AND CO2 FLUX – LEGS 1 AND 2 39 2.1 Introduction 39 2.2 Methodology 40 2.3 Preliminary results 44 3 SEA ICE, REMOTE SENSING AND MARGINAL ICE ZONE – LEG 1 45 3.1 Introduction 45 3.2 Methodology 45 3.3 Preliminary results 60 4 MOORING PROGRAM – LEGS 1 AND 2A (AMUNDSEN) AND BAYSYS (RADISSON) 62 4.1 Introduction 62 4.2 Methodology 64 4.3 Comments and recommendations 86 5 CTD-ROSETTE, ADCP AND THERMOSALINOGRAPH – LEGS 1 AND 2 88 5.1 CTD-Rosette 88 5.2 Preliminary results CTD-Rosette (Leg 2b – Labrador fjords) 90 5.3 ADCP and thermosalinograph (TSG) 92 6 SELF-CONTAINED AUTONOMOUS MICROPROFILER (SCAMP) – LEGS 1 AND 2 93 6.1 Introduction 93 6.2 Methodology 93 6.3 Preliminary results 95 7 CARBON FLUXES USING DRIFTING SEDIMENT TRAPS – LEGS 1 AND 2A 97 7.1 Introduction 97 7.2 Methodology 97 8 NUTRIENTS, NITROGEN CYCLING AND ECOPHYSIOLOGY OF PHYTOPLANKON – LEGS 1 AND 2A 100 8.1 Introduction 100 8.2 Methodology 101 8.3 Preliminary results 105 9 MOLECULAR MICROBIAL BIODIVERSITY OF ARCTIC SEAS – LEGS 1 AND 2A 108 9.1 Introduction 108 9.2 Methodology 109 9.3 Preliminary results 114 10 MICROBIAL PROGRAM - LEGS 1 AND 2A 115 10.1 Introduction 115 10.2 Methodology 116 10.3 Preliminary results 120 11 THORIUM RADIONUCLIDE PROGRAM – LEG 1 122 11.1 Introduction 122 11.2 Methodology 122 11.3 Preliminary results 124 12 PHYTOPLANKTON AND PRIMARY PRODUCTION – LEGS 1 AND 2A 125 12.1 Introduction 125 12.2 Methodology 126 13 ZOOPLANKTON AND ICHTYOPLANKTON – LEGS 1 AND 2A 129 13.1 Introduction 129 13.2 Methodology 130 13.3 Preliminary results 137 14 CONTAMINANTS SAMPLING PROGRAM – LEGS 1 AND 2 141 14.1 Introduction 141 14.2 Methodology 143 14.3 Preliminary results 149 iii 15 BIOGEOCHEMICAL CYCLING OF MERCURY – LEG 1 150 15.1 Introduction 150 15.2 Methodology 151 15.3 Preliminary results 152 16 SEAFLOOR MAPPING – LEGS 1 AND 2 153 16.1 Introduction 153 16.2 Methodology 156 16.3 Preliminary results 159 16.4 Comments and recommendations (Leg 2) 175 17 GEOLOGY AND PALEONTOLOGY – LEGS 1 AND 2B 177 17.1 Introduction 177 17.2 Methodology 179 17.3 Preliminary results (Leg 2a) 187 17.4 Preliminary results (Leg 2b) 189 17.5 Comments and recommendations (Leg 1 only) 191 18 CANADA’S ARCTIC WATERS IN INTERNATIONAL LAW AND DIPLOMACY – LEG 2A 193 18.1 Introduction 193 18.2 Project output to date 194 18.3 Amundsen contribution to the project 194 19 NAVIGATION POTENTIAL IN CANADIAN ARCTIC WATERS – LEGS 1 AND 2A 196 19.1 Assessment of opportunities and risks for a risk-averse industry 196 APPENDIX 1 – LIST OF STATIONS SAMPLED DURING THE 2006 ARCTICNET EXPEDITION 198 APPENDIX 2 – SCIENTIFIC LOG OF ACTIVITIES CONDUCTED DURING THE 2006 ARCTICNET EXPEDITION 202 APPENDIX 3 – CTD LOGBOOK FOR THE 2006 ARCTICNET EXPEDITION 241 APPENDIX 4 – LIST OF SCIENCE PARTICIPANTS ON THE 2006 ARCTICNET EXPEDITION 248 iv List of Figures PART I – OVERVIEW AND SYNOPSIS OF OPERATIONS Figure 1.1. Map of the Canadian High Arctic showing the CCGS Amundsen ship track and the location of stations for the two legs of the 2006 ArcticNet Expedition. Stations and mooring sites in Hudson Bay were visited by the CCGS Pierre Radisson as part of the BaySys expedition. ............................................................................................................................................. 3 Figure 1.2. Map of northern Baffin Bay, Nares Strait and Lancaster Sound showing the ship track and the location of stations sampled by the CCGS Amundsen during the second portion of Leg 1 of the 2006 ArcticNet Expedition. Stations were also visited in the Labrador Sea and Hudson Strait during the first segment of Leg 1 (see Figure 2.1 in Section 2 below). ................................ 6 Figure 1.3. Map of the Canadian Arctic Archipelago (Northwest Passage) showing the ship track and the location of stations sampled by the CCGS Amundsen during the third portion of Leg 1 of the 2006 ArcticNet Expedition. Not shown on this map is the location of stations visited in the same region on the eastward route during Leg 2a (see Figure 1.5 below). ................................... 7 Figure 1.4. Map of the Amundsen Gulf and Beaufort Sea showing the ship track and the location of stations sampled by the CCGS Amundsen during the first segment of Leg 2a of the 2006 ArcticNet Expedition. ......................................................................................................... 8 Figure 1.5. Map of the Canadian Arctic Archipelago (Northwest Passage) showing the ship track and the location of stations visited by the CCGS Amundsen during the second portion of Leg 2a of the 2006 ArcticNet Expedition.............................................................................................. 9 Figure 1.6. Map of the northern Labrador coast and Labrador Sea showing the ship track and the location of stations sampled in three northern Labrador fjords by the CCGS Amundsen during Leg 2b of the 2006 ArcticNet Expedition. Also shown on this map is the northward route taken by the Amundsen during Leg 1 (see also Figure 2.1 below). .................................................... 10 Figure 1.7. Map of Hudson Bay showing the location of stations and mooring sites visited in Hudson Bay by the CCGS Pierre Radisson during the BaySys expedition as part of the 2006 ArcticNet Expedition. ..................................................................................................................... 11 Figure 2.1. Map of the Labrador Sea showing the cruise track and the location of stations sampled in the Labrador Sea and Hudson Strait Slope during the first portion of Leg 1 (22 to 31 August). Also shown is the Amundsen cruise track for Leg 2b. ............................................................ 14 Figure 2.2. Map of northern Baffin Bay and Nares Strait with the location and type of stations sampled from 1 September to 21 September 2006 during Leg 1 of the ArcticNet Expedition onboard the CCGS Amundsen. .......................................................................................... 15 Figure 2.3. Map of the Canadian Arctic Archipelago (westward route through McClintock Channel) showing the location and type of stations sampled from 20 September to 27 September 2006 during Leg 1 of the ArcticNet Expedition onboard the CCGS Amundsen................................... 16 Figure 2.4. Relative amount of effort (in number of hours) spent on scientific activities during Leg 1. The graph does not include activities which are conducted in parallel with other operations. ....... 17 Figure 3.1. map of the Amundsen Gulf and the Beaufort Sea showing the location and type of stations sampled from 29 September to 20 October 2006 during Leg 2a of the ArcticNet Expedition onboard the CCGS Amundsen. .......................................................................... 21 Figure 3.2. Map of the Canadian Arctic Archipelago (eastward route through Bellot Strait, Gulf of Boothia, Fury and Hecla Straits), Foxe Basin and Hudson Strait showing the location and type of stations sampled from 20 October to 29 October 2006 during Leg 2a of the ArcticNet Expedition onboard the CCGS Amundsen. .......................................................................... 22 Figure 4.1. Map of the Labrador coast showing the location and type of stations in Nachvak fjord (Stations 600-604), Saglek fjord (Stations 610-617) and Anaktalak Bay (Stations 620-624) sampled from 1 to 4 November 2006 during Leg 2b of the ArcticNet Expedition onboard the CCGS Amundsen. ........................................................................................................... 27 v Figure 5.1. Map of Hudson Bay showing the location and type of stations sampled from 12 September
Recommended publications
  • Transits of the Northwest Passage to End of the 2019 Navigation Season Atlantic Ocean ↔ Arctic Ocean ↔ Pacific Ocean
    TRANSITS OF THE NORTHWEST PASSAGE TO END OF THE 2019 NAVIGATION SEASON ATLANTIC OCEAN ↔ ARCTIC OCEAN ↔ PACIFIC OCEAN R. K. Headland and colleagues 12 December 2019 Scott Polar Research Institute, University of Cambridge, Lensfield Road, Cambridge, United Kingdom, CB2 1ER. <[email protected]> The earliest traverse of the Northwest Passage was completed in 1853 but used sledges over the sea ice of the central part of Parry Channel. Subsequently the following 314 complete maritime transits of the Northwest Passage have been made to the end of the 2019 navigation season, before winter began and the passage froze. These transits proceed to or from the Atlantic Ocean (Labrador Sea) in or out of the eastern approaches to the Canadian Arctic archipelago (Lancaster Sound or Foxe Basin) then the western approaches (McClure Strait or Amundsen Gulf), across the Beaufort Sea and Chukchi Sea of the Arctic Ocean, through the Bering Strait, from or to the Bering Sea of the Pacific Ocean. The Arctic Circle is crossed near the beginning and the end of all transits except those to or from the central or northern coast of west Greenland. The routes and directions are indicated. Details of submarine transits are not included because only two have been reported (1960 USS Sea Dragon, Capt. George Peabody Steele, westbound on route 1 and 1962 USS Skate, Capt. Joseph Lawrence Skoog, eastbound on route 1). Seven routes have been used for transits of the Northwest Passage with some minor variations (for example through Pond Inlet and Navy Board Inlet) and two composite courses in summers when ice was minimal (transits 149 and 167).
    [Show full text]
  • Canadian Arctic Through-Flow 2012 Cruise to Nares Strait
    Canadian Arctic Through-flow 2012 Cruise to Nares Strait CCGS Henry Larsen August 2-17, 2012 Institute of Ocean Sciences Cruise 2012-20 Humfrey Melling – Chief Scientist Fisheries & Oceans Canada Collaborating Institutions: Institute of Ocean Sciences, University of Delaware, Oxford University, Danish Technical University, Scottish Association for Marine Science 1 Cover photo, courtesy of Jason Box: View looking south across the Petermann ice shelf towards Joe Island, Kennedy Channel and Ellesmere Island at the horizon. Note the small ice-shelf fragments in the foreground and cracks within the protruding lobe of the ice . The photograph taken in 2009, before the large ice islands calved from the shelf in August 2010 and again in July 2012. 2 Report on the Scientific Cruise of CCGS Henry Larsen, August 2012 Canadian Arctic Through-flow CCGS Henry Larsen in Nares Strait August 2-17, 2012 Overview The Canadian Arctic Through-flow (CAT) study embodies ten years’ effort within Canada and the international community to measure flows of seawater and ice through the Canadian Archipelago, between the Arctic and the Atlantic Oceans. CATs is the outgrowth of a pilot effort, the Arctic Canada Watch, established in 1997. Moorings enabling year-round measurements were first placed in western Lancaster Sound and Cardigan Strait in 1998. These carried instruments to measure current, temperature and salinity and utilized innovations to address the unique challenges of observing: 1) current direction near the geomagnetic pole; 2) salinity within the hazardous 30-m zone beneath drifting ice pack. These early installations have been maintained and augmented since 1998. In 2003, a large array of instruments was installed across the third principal path for Canadian Arctic through-flow, Nares Strait.
    [Show full text]
  • Paleocene Alkaline Volcanism in the Nares Strait Region Related to Strike-Slip Tectonics
    Paleocene Alkaline Volcanism in the Nares Strait Region Related to Strike-slip Tectonics Solveig Estrada & Detlef Damaske Federal Institute for Geosciences and Natural Resources (BGR), Hannover, Germany ([email protected]) The tectonic development of the North Atlantic, the Labrador Sea/Baffin Bay and the Eurasian Basin of Arctic Ocean led to relative movements between the Greenland Plate and the North American Plate. There has been a debate for many years, whether the Nares Strait between northwest Greenland and Ellesmere Island marks an ancient plate boundary in terms of a left-lateral transform fault (Wegener Fault) or whether there was no movement between Greenland and Ellesmere Island at all. New data were acquired during joint German-Canadian geological field work on northeast Ellesmere Island 1998-2000 (Mayr 2008), followed in 2001 by a geoscience cruise in Nares Strait (Tessensohn et al. 2006). Indications for sinistral strike-slip movements followed by compressive tectonics were found at the western margin of northern Nares Strait (Saalmann et al. 2005). Paleogene basins on Judge Daly Promontory, northeast Ellesmere Island, are bounded by a complex pattern of strike-slip and thrust faults. The clastic sediments in the basins are rich in volcanogenic material. Volcanic pebbles within the Cape Back basin near Nares Strait are derived from lava flows and ignimbrites of a continental rift-related, strongly differentiated, highly incompatible element enriched, alkaline volcanic suite (Estrada et al. 2009). 40Ar/39Ar amphibole and alkali feldspar ages indicate that volcanism was active around 61–58 Ma and was probably contemporaneous with sedimentation within the Paleogene pull-apart basins on Judge Daly Promontory formed by sinistral strike-slip tectonics parallel to the present-day Nares Strait.
    [Show full text]
  • Seismic Reflection Profiles from Kane to Hall Basin, Nares Strait: Evidence for Faulting
    Polarforschung 74 (1-3), 21 – 39, 2004 (erschienen 2006) Seismic Reflection Profiles from Kane to Hall Basin, Nares Strait: Evidence for Faulting by H. Ruth Jackson1, Tim Hannon1, Sönke Neben2, Karsten Piepjohn2 and Tom Brent3 Abstract: Three major tectonic boundaries are predicted to be present beneath durch eine folgende kompressive Phase reaktiviert wurde. Als Arbeitshypo- the waters of this segment of Nares Strait: (1) the orogenic front of the Paleo- these fassen wir die oberflächennahen Teile dieses Systems als Stirn der Plat- zoic Ellesmerian Foldbelt between thrust sheets on Ellesmere Island and flat- tengrenze zwischen Nordamerika und Grönland auf. lying foreland rocks on Greenland, (2) the supposed sinistral strike-slip plate boundary of Paleocene age between the Ellemere Island section of the North America plate and the Greenland plate, and (3) the orogenic front of the Eocene to Oligocene Eurekan Foldbelt that must lie between thrust tectonics INTRODUCTION on Ellesmere Island and undeformed rocks of Greenland. To understand this complicated situation and to look for direct evidence of the plate boundary, The Late Cretaceous and Tertiary deformation on Ellesmere new seismic reflection profiles were collected and, together with industry data in the south, interpreted. The profiles are clustered in three areas controlled by Island (Fig. 1) called the Eurekan Orogeny has been attributed the distribution of the sea ice. Bathymetry is used to extrapolate seismic to the counter clockwise rotation of Greenland (e.g., OKULITCH features with a topographic expression between the regions. Based on high- & TRETTIN 1991). However reconciling the geology on oppo- resolution boomer and deeper penetration airgun profiles five seismic units are mapped.
    [Show full text]
  • Jökulhlaups in Skaftá: a Study of a Jökul- Hlaup from the Western Skaftá Cauldron in the Vatnajökull Ice Cap, Iceland
    Jökulhlaups in Skaftá: A study of a jökul- hlaup from the Western Skaftá cauldron in the Vatnajökull ice cap, Iceland Bergur Einarsson, Veðurstofu Íslands Skýrsla VÍ 2009-006 Jökulhlaups in Skaftá: A study of jökul- hlaup from the Western Skaftá cauldron in the Vatnajökull ice cap, Iceland Bergur Einarsson Skýrsla Veðurstofa Íslands +354 522 60 00 VÍ 2009-006 Bústaðavegur 9 +354 522 60 06 ISSN 1670-8261 150 Reykjavík [email protected] Abstract Fast-rising jökulhlaups from the geothermal subglacial lakes below the Skaftá caul- drons in Vatnajökull emerge in the Skaftá river approximately every year with 45 jökulhlaups recorded since 1955. The accumulated volume of flood water was used to estimate the average rate of water accumulation in the subglacial lakes during the last decade as 6 Gl (6·106 m3) per month for the lake below the western cauldron and 9 Gl per month for the eastern caul- dron. Data on water accumulation and lake water composition in the western cauldron were used to estimate the power of the underlying geothermal area as ∼550 MW. For a jökulhlaup from the Western Skaftá cauldron in September 2006, the low- ering of the ice cover overlying the subglacial lake, the discharge in Skaftá and the temperature of the flood water close to the glacier margin were measured. The dis- charge from the subglacial lake during the jökulhlaup was calculated using a hypso- metric curve for the subglacial lake, estimated from the form of the surface cauldron after jökulhlaups. The maximum outflow from the lake during the jökulhlaup is esti- mated as 123 m3 s−1 while the maximum discharge of jökulhlaup water at the glacier terminus is estimated as 97 m3 s−1.
    [Show full text]
  • Chapter 8 Polar Bear Harvesting in Baffin Bay and Kane Basin: a Summary of Historical Harvest and Harvest Reporting, 1993 to 2014
    Chapter 8 SWG Final Report CHAPTER 8 POLAR BEAR HARVESTING IN BAFFIN BAY AND KANE BASIN: A SUMMARY OF HISTORICAL HARVEST AND HARVEST REPORTING, 1993 TO 2014 KEY FINDINGS Both Canada (Nunavut) and Greenland harvest from the shared subpopulations of polar • bears in Baffin Bay and Kane Basin. During 1993-2005 (i.e., before quotas were introduced in Greenland) the combined • annual harvest averaged 165 polar bears (range: 120-268) from the Baffin Bay subpopulation and 12 polar bears (range: 6-26) from Kane Basin (for several of the years, harvest reported from Kane Basin was based on an estimate). During 2006-2014 the combined annual harvest averaged 161 (range: 138-176) from • Baffin Bay and 6 (range: 3-9) polar bears from Kane Basin. Total harvest peaked between 2002 and 2005 coinciding with several events in harvest • reporting and harvest management in both Canada and Greenland. In Baffin Bay the sex ratio of the combined harvest has remained around 2:1 (male: • females) with an annual mean of 35% females amongst independent bears. In Kane Basin the sex composition of the combined harvest was 33% females overall for • the period 1993-2014. The estimated composition of the harvest since the introduction of a quota in Greenland is 44% female but the factual basis for estimation of the sex ratio in the harvest is weak. In Greenland the vast majority of bears are harvested between January and June in Baffin • Bay and Kane Basin whereas in Nunavut ca. 40% of the harvest in Baffin Bay is in the summer to fall (August – November) while bears are on or near shore.
    [Show full text]
  • Canadian Coast Guard Arctic Operations Julie Gascon - Assistant Commissioner Canadian Coast Guard, Central & Arctic Region
    Unclassified Canadian Coast Guard Arctic Operations Julie Gascon - Assistant Commissioner Canadian Coast Guard, Central & Arctic Region Naval Association of Canada Ottawa, ON May 1, 2017 1 Canadian Coast Guard (CCG): Who We Are and What We Do Operating as Canada’s only Deliver programs and services to the national civilian fleet, we population to ensure safe and accessible provide a wide variety of waterways and to facilitate maritime programs and services to commerce; the population and to the maritime industry on important levels: Provide vessels and helicopters to enable fisheries enforcement activities, and the on-water science research for Fisheries and Oceans Canada and other science departments; and Support maritime security activities. 2 Canadian Coast Guard: Regional Boundaries • Western Region: Pacific Ocean, Great Slave Lake, Mackenzie River and Lake Winnipeg • Central & Arctic Region: Hudson Bay, Great Lakes, St. Lawrence River, Gulf of St. Lawrence (Northern Area), and Arctic Ocean • Atlantic Region : Atlantic Ocean, Gulf of St. Lawrence (Southern Area), and Bay of Fundy 3 Central and Arctic Region: Fact Sheet The Central and Arctic Region covers: - St. Lawrence River, Gulf of St. Lawrence (Northern Area), Great Lakes, Hudson Bay and the Arctic coast up to Alaska - Population of approx 21.5 million inhabitants - Nearly 3,000,000 km2 of water area • A regional office and 10 operational bases • 39 vessels • 15 SAR lifeboat stations • 12 inshore rescue stations • air cushion vehicles 2 Nunavut • 8 helicopters • 4,627 floating aids • 2,191 fixed aids • 5 MCTS centres Quebec Ontario Quebec Base Montreal, Quebec Sarnia Office 4 Presentation Overview The purpose of this presentation is to: 1.
    [Show full text]
  • Arctic Marine Transport Workshop 28-30 September 2004
    Arctic Marine Transport Workshop 28-30 September 2004 Institute of the North • U.S. Arctic Research Commission • International Arctic Science Committee Arctic Ocean Marine Routes This map is a general portrayal of the major Arctic marine routes shown from the perspective of Bering Strait looking northward. The official Northern Sea Route encompasses all routes across the Russian Arctic coastal seas from Kara Gate (at the southern tip of Novaya Zemlya) to Bering Strait. The Northwest Passage is the name given to the marine routes between the Atlantic and Pacific oceans along the northern coast of North America that span the straits and sounds of the Canadian Arctic Archipelago. Three historic polar voyages in the Central Arctic Ocean are indicated: the first surface shop voyage to the North Pole by the Soviet nuclear icebreaker Arktika in August 1977; the tourist voyage of the Soviet nuclear icebreaker Sovetsky Soyuz across the Arctic Ocean in August 1991; and, the historic scientific (Arctic) transect by the polar icebreakers Polar Sea (U.S.) and Louis S. St-Laurent (Canada) during July and August 1994. Shown is the ice edge for 16 September 2004 (near the minimum extent of Arctic sea ice for 2004) as determined by satellite passive microwave sensors. Noted are ice-free coastal seas along the entire Russian Arctic and a large, ice-free area that extends 300 nautical miles north of the Alaskan coast. The ice edge is also shown to have retreated to a position north of Svalbard. The front cover shows the summer minimum extent of Arctic sea ice on 16 September 2002.
    [Show full text]
  • Research Cruise Report: Mission HLY031
    Research Cruise Report: Mission HLY031 Conducted aboard USCGC Healy In Northern Baffi n Bay and Nares Strait 21 July –16 August 2003 Project Title: Variability and Forcing of Fluxes through Nares Strait and Jones Sound: A Freshwater Emphasis Sponsored by the US National Science Foundation, Offi ce of Polar Programs, Arctic Division Table of Contents Introduction by Chief Scientist . 4 Science Program Summary . 6 Science Party List . 7 Crew List . 8 Science Component Reports CTD-Rosette Hydrography . 9 Internally recording CTD . 29 Kennedy Channel Moorings . 33 Pressure Array . 41 Shipboard ADCP . 47 Bi-valve Retrieval . 51 Coring . 55 Seabeam Mapping . 65 Aviation Science Report . 71 Ice Report . 79 Weather Summary . 91 Inuit Perspective . 95 Photojournalist Perspective . 101. Website Log . 105 Chief Scientist Log . 111 Recommendations . .125 Introduction Dr. Kelly Kenison Falkner Chief Scientist Oregon State University In the very early hours of July 17, 2003, I arrived at collected via the ship’s Seabeam system and the underway the USCGC Healy moored at the fueling pier in St. John’s thermosalinograph system was put to good use throughout Newfoundland, Canada to assume my role as chief scientist much of the cruise. for an ambitious interdisciplinary mission to Northern Part of our success can be attributed to luck with Mother Baffi n Bay and Nares St. This research cruise constitutes Nature. Winds and ice worked largely in our favor as we the inaugural fi eld program of a fi ve year collaborative wound our way northward. Our winds were generally research program entitled Variability and Forcing of moderate and out of the south and the ice normal to light.
    [Show full text]
  • Perceived Implications of Privatization for Canadian Coast Guard Services, Principally Arctic Icebreaking
    Perceived Implications Of Privatization For Canadian Coast Guard Services, Principally Arctic Icebreaking by James Parsons A thesis submitted to the University of Plymouth in partial fulfilment for the degree of DOCTOR OF PHILOSOPHY International Shipping and Logistics Group School of Management, Plymouth Business School August 2009 Abstract James Parsons Perceived Implications Of Privatization For Canadian Coast Guard Services, Principally Arctic Icebreaking Climate change, with the possibility of an ice free Arctic ocean by 2015, has generated a renewed interest in the Arctic. This interest is being driven by the possibility of easier access to the abundant supply of resources such as oil, gas, minerals, and fisheries. Interest in Arctic tourism is also growing. Retreating sea ice will provide opportunities to avail of shorter routes for maritime traffic to and from Asia, North America, and Asia via the Arctic Ocean and Northwest Passage. In addition, the rate of population growth of local inhabitants in the Canadian Arctic is the fastest in Canada and one of the fastest in the world. A growing population will increase the demand for sealift resupply to Canada's northern communities. This work presents the first attempt to examine the role of privatization of icebreaking services in light of the present and projected shortages of infrastructure to support development in the Arctic. A unique combination of multiple methods within marine transportation, comprising of Delphi, grounded theory, and quantitative survey, is applied to investigate the potential for private involvement in the delivery of icebreaking services in the Canadian Arctic. This includes a novel application of Strauss and Corbin's Grounded Theory approach to develop hypotheses and relationships grounded in expert opinion.
    [Show full text]
  • Re-Evaluation of Strike-Slip Displacements Along and Bordering Nares Strait
    Polarforschung 74 (1-3), 129 – 160, 2004 (erschienen 2006) In Search of the Wegener Fault: Re-Evaluation of Strike-Slip Displacements Along and Bordering Nares Strait by J. Christopher Harrison1 Abstract: A total of 28 geological-geophysical markers are identified that lich der Bache Peninsula und Linksseitenverschiebungen am Judge-Daly- relate to the question of strike slip motions along and bordering Nares Strait. Störungssystem (70 km) und schließlich die S-, später SW-gerichtete Eight of the twelve markers, located within the Phanerozoic orogen of Kompression des Sverdrup-Beckens (100 + 35 km). Die spätere Deformation Kennedy Channel – Robeson Channel region, permit between 65 and 75 km wird auf die Rotation (entgegen dem Uhrzeigersinn) und ausweichende West- of sinistral offset on the Judge Daly Fault System (JDFS). In contrast, eight of drift eines semi-rigiden nördlichen Ellesmere-Blocks während der Kollision nine markers located in Kane Basin, Smith Sound and northern Baffin Bay mit der Grönlandplatte zurückgeführt. indicate no lateral displacement at all. Especially convincing is evidence, presented by DAMASKE & OAKEY (2006), that at least one basic dyke of Neoproterozoic age extends across Smith Sound from Inglefield Land to inshore eastern Ellesmere Island without any recognizable strike slip offset. INTRODUCTION These results confirm that no major sinistral fault exists in southern Nares Strait. It is apparent to both earth scientists and the general public To account for the absence of a Wegener Fault in most parts of Nares Strait, that the shape of both coastlines and continental margins of the present paper would locate the late Paleocene-Eocene Greenland plate boundary on an interconnected system of faults that are 1) traced through western Greenland and eastern Arctic Canada provide for a Jones Sound in the south, 2) lie between the Eurekan Orogen and the Precam- satisfactory restoration of the opposing lands.
    [Show full text]
  • December 23, 1903
    menatn l SUBSCRIPTION PRICK. #2.00 PER TlAR. mod!| i ENTf RED AS SECOND CLAS8 MATTER 1 XLIX, Vol. I IP PAID IN ADVANCE, #1.50 1903. No. ELLSWORTH, MAINE, WEDNESDAY AFTERNOON, DECEMBER 23, f AT THE ELLSWORTH POST OF-ICE. { 51. 'aubertMcmente. LOCAL AFFAIRS George F. Hank ell; delegate to State en- TWO BIO FIRES. campment, James L. Cook; alternate, W. C. R. R, SOLD THE OLD RELIABLE Dorephus L. Fields. How Ellsworth Suffered in the Days SKW A DVKKTISEM ENTS THIS WEKK. PAID THE of Misses Annie and Helen Mitchell, ac- $2,300,000 FOR DOWN Long Ago. Tbe recent disastrous at In bankruptcy—Est Chas II White. companied by their brother Asa, have EAST ROAD. conflagration Waller H Brooks—Notice of foreclosure. Cherryfield brings to the minds of Elia- Hancock George H Waaso<i—Notice of foreclosure. gone to Massachusetts and New Hamp- County Savings Bank, worth’s oldest inhabitants two serious Han Fair A Co *s’n—Stockholders’ meeting. shire for a short visit among relatives and ONLY TWENTY PERSONS PRESENT AND First Nat’I hank—'Stockholders* meeting. conflagrations in Ellsworth’s history, one Flluworth Loan A Ass’n—Annual friends. ONLY ONE BID—PROMPTLY ACCEPTED ORGANIZED MARCH Building of which 17, 1873, I®* '»ng. occurred on Dec. 12, 1845, the Esoteric lodge will work the third de- AND FORFEIT DEPOSITED. In bankruptcy— K"t Calvin H Norris. other nine years later, on Dec. 24, 1851. has semi-annual In Kst Harvey W Hodgkins. on four candidates this An paid regular dividends amounting to *201,*11.01 bankruptcy— gree evening.
    [Show full text]