Climate Change, Ice Conditions and Reproduction in an Arctic Nesting
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Arctic Seabirds and Shrinking Sea Ice: Egg Analyses Reveal the Importance
www.nature.com/scientificreports OPEN Arctic seabirds and shrinking sea ice: egg analyses reveal the importance of ice-derived resources Fanny Cusset1*, Jérôme Fort2, Mark Mallory3, Birgit Braune4, Philippe Massicotte1 & Guillaume Massé1,5 In the Arctic, sea-ice plays a central role in the functioning of marine food webs and its rapid shrinking has large efects on the biota. It is thus crucial to assess the importance of sea-ice and ice-derived resources to Arctic marine species. Here, we used a multi-biomarker approach combining Highly Branched Isoprenoids (HBIs) with δ13C and δ15N to evaluate how much Arctic seabirds rely on sea-ice derived resources during the pre-laying period, and if changes in sea-ice extent and duration afect their investment in reproduction. Eggs of thick-billed murres (Uria lomvia) and northern fulmars (Fulmarus glacialis) were collected in the Canadian Arctic during four years of highly contrasting ice conditions, and analysed for HBIs, isotopic (carbon and nitrogen) and energetic composition. Murres heavily relied on ice-associated prey, and sea-ice was benefcial for this species which produced larger and more energy-dense eggs during icier years. In contrast, fulmars did not exhibit any clear association with sympagic communities and were not impacted by changes in sea ice. Murres, like other species more constrained in their response to sea-ice variations, therefore appear more sensitive to changes and may become the losers of future climate shifts in the Arctic, unlike more resilient species such as fulmars. Sea ice plays a central role in polar marine ecosystems; it drives the phenology of primary producers that con- stitute the base of marine food webs. -
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. -
Transits of the Northwest Passage to End of the 2020 Navigation Season Atlantic Ocean ↔ Arctic Ocean ↔ Pacific Ocean
TRANSITS OF THE NORTHWEST PASSAGE TO END OF THE 2020 NAVIGATION SEASON ATLANTIC OCEAN ↔ ARCTIC OCEAN ↔ PACIFIC OCEAN R. K. Headland and colleagues 7 April 2021 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 starting in the Pacific Ocean to reach the Atlantic Oceam, but used sledges over the sea ice of the central part of Parry Channel. Subsequently the following 319 complete maritime transits of the Northwest Passage have been made to the end of the 2020 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 (marked ‘cp’). -
Who Discovered the Northwest Passage? Janice Cavell1
ARCTIC VOL. 71, NO.3 (SEPTEMBER 2018) P.292 – 308 https://doi.org/10.14430/arctic4733 Who Discovered the Northwest Passage? Janice Cavell1 (Received 31 January 2018; accepted in revised form 1 May 2018) ABSTRACT. In 1855 a parliamentary committee concluded that Robert McClure deserved to be rewarded as the discoverer of a Northwest Passage. Since then, various writers have put forward rival claims on behalf of Sir John Franklin, John Rae, and Roald Amundsen. This article examines the process of 19th-century European exploration in the Arctic Archipelago, the definition of discovering a passage that prevailed at the time, and the arguments for and against the various contenders. It concludes that while no one explorer was “the” discoverer, McClure’s achievement deserves reconsideration. Key words: Northwest Passage; John Franklin; Robert McClure; John Rae; Roald Amundsen RÉSUMÉ. En 1855, un comité parlementaire a conclu que Robert McClure méritait de recevoir le titre de découvreur d’un passage du Nord-Ouest. Depuis lors, diverses personnes ont avancé des prétentions rivales à l’endroit de Sir John Franklin, de John Rae et de Roald Amundsen. Cet article se penche sur l’exploration européenne de l’archipel Arctique au XIXe siècle, sur la définition de la découverte d’un passage en vigueur à l’époque, de même que sur les arguments pour et contre les divers prétendants au titre. Nous concluons en affirmant que même si aucun des explorateurs n’a été « le » découvreur, les réalisations de Robert McClure méritent d’être considérées de nouveau. Mots clés : passage du Nord-Ouest; John Franklin; Robert McClure; John Rae; Roald Amundsen Traduit pour la revue Arctic par Nicole Giguère. -
Canadian Arctic Tide Measurement Techniques and Results
International Hydrographie Review, Monaco, LXIII (2), July 1986 CANADIAN ARCTIC TIDE MEASUREMENT TECHNIQUES AND RESULTS by B.J. TAIT, S.T. GRANT, D. St.-JACQUES and F. STEPHENSON (*) ABSTRACT About 10 years ago the Canadian Hydrographic Service recognized the need for a planned approach to completing tide and current surveys of the Canadian Arctic Archipelago in order to meet the requirements of marine shipping and construction industries as well as the needs of environmental studies related to resource development. Therefore, a program of tidal surveys was begun which has resulted in a data base of tidal records covering most of the Archipelago. In this paper the problems faced by tidal surveyors and others working in the harsh Arctic environment are described and the variety of equipment and techniques developed for short, medium and long-term deployments are reported. The tidal characteris tics throughout the Archipelago, determined primarily from these surveys, are briefly summarized. It was also recognized that there would be a need for real time tidal data by engineers, surveyors and mariners. Since the existing permanent tide gauges in the Arctic do not have this capability, a project was started in the early 1980’s to develop and construct a new permanent gauging system. The first of these gauges was constructed during the summer of 1985 and is described. INTRODUCTION The Canadian Arctic Archipelago shown in Figure 1 is a large group of islands north of the mainland of Canada bounded on the west by the Beaufort Sea, on the north by the Arctic Ocean and on the east by Davis Strait, Baffin Bay and Greenland and split through the middle by Parry Channel which constitutes most of the famous North West Passage. -
Arctic Cephalopod Distributions and Their Associated Predatorspor 146 209..227 Kathleen Gardiner & Terry A
Arctic cephalopod distributions and their associated predatorspor_146 209..227 Kathleen Gardiner & Terry A. Dick Biological Sciences, University of Manitoba, Winnipeg, Manitoba R3T 2N2, Canada Keywords Abstract Arctic Ocean; Canada; cephalopods; distributions; oceanography; predators. Cephalopods are key species of the eastern Arctic marine food web, both as prey and predator. Their presence in the diets of Arctic fish, birds and mammals Correspondence illustrates their trophic importance. There has been considerable research on Terry A. Dick, Biological Sciences, University cephalopods (primarily Gonatus fabricii) from the north Atlantic and the west of Manitoba, Winnipeg, Manitoba R3T 2N2, side of Greenland, where they are considered a potential fishery and are taken Canada. E-mail: [email protected] as a by-catch. By contrast, data on the biogeography of Arctic cephalopods are doi:10.1111/j.1751-8369.2010.00146.x still incomplete. This study integrates most known locations of Arctic cepha- lopods in an attempt to locate potential areas of interest for cephalopods, and the predators that feed on them. International and national databases, museum collections, government reports, published articles and personal communica- tions were used to develop distribution maps. Species common to the Canadian Arctic include: G. fabricii, Rossia moelleri, R. palpebrosa and Bathypolypus arcticus. Cirroteuthis muelleri is abundant in the waters off Alaska, Davis Strait and Baffin Bay. Although distribution data are still incomplete, groupings of cephalopods were found in some areas that may be correlated with oceanographic variables. Understanding species distributions and their interactions within the ecosys- tem is important to the study of a warming Arctic Ocean and the selection of marine protected areas. -
Arctic / Sub-Arctic Ocean Fluxes Study
ARCTIC / SUB-ARCTIC OCEAN FLUXES STUDY Report of the 3rd meeting of ASOF International Scientific Steering Group 25-26 October 2003 Seattle, USA February 2004 1 Table of Contents 1. Introduction 3 2. ASOF-WEST Status and Plans 4 2.1 Towards an Integrated Strategy 4 2.2 Pacific Gateway to the Arctic 5 2.3 Flow through the Canadian Arctic Archipelago: What do we know? 6 2.4 BIO/Canada Contribution to ASOF-WEST 8 2.5 The Labrador Sea at Half a Knot on Half a Watt 9 2.6 Fluxes Variability in Davis Strait 10 2.7 Variability and Forcing of Fluxes through Nares Strait and Jones Sound: a 11 Freshwater Emphasis 2.8 The Joint Western Arctic Climate Study: a Strategic Vision 13 2.9 Barium as a Freshwater Tracer in the Arctic 14 2.10 Modelling Arctic-North Atlantic Exchange and Decadal Variability 15 2.11 Northern Hemisphere Sea-ice Variability and its linkage to the NAO and 17 ENSO 3. Task 5. Overflows and Storage Basins 18 4. ASOF-EAST Status and Plans 19 4.1 Future Strategy 20 5. Task 2 and ASOF-EC(North) Progress and Plans 23 6. Task 3: Freshwater Fluxes 25 6.1 Freshwater arrays along Greenland slope 25 7. Task 1 and ASOF Meridional Overturning Exchanges with the Nordic Seas 26 8. From MAIA to ASOF 28 9. Task 7. Numerical Experiments Group 29 9.1 An overview of the large-scale modelling activity in Bergen 30 9.2 Modelled Arctic-Subarctic Ocean Fluxes during 1979-2001 32 10. -
Canada's Arctic Marine Atlas
Lincoln Sea Hall Basin MARINE ATLAS ARCTIC CANADA’S GREENLAND Ellesmere Island Kane Basin Nares Strait N nd ansen Sou s d Axel n Sve Heiberg rdr a up Island l Ch ann North CANADA’S s el I Pea Water ry Ch a h nnel Massey t Sou Baffin e Amund nd ISR Boundary b Ringnes Bay Ellef Norwegian Coburg Island Grise Fiord a Ringnes Bay Island ARCTIC MARINE z Island EEZ Boundary Prince i Borden ARCTIC l Island Gustaf E Adolf Sea Maclea Jones n Str OCEAN n ait Sound ATLANTIC e Mackenzie Pe Ball nn antyn King Island y S e trait e S u trait it Devon Wel ATLAS Stra OCEAN Q Prince l Island Clyde River Queens in Bylot Patrick Hazen Byam gt Channel o Island Martin n Island Ch tr. Channel an Pond Inlet S Bathurst nel Qikiqtarjuaq liam A Island Eclipse ust Lancaster Sound in Cornwallis Sound Hecla Ch Fitzwil Island and an Griper nel ait Bay r Resolute t Melville Barrow Strait Arctic Bay S et P l Island r i Kel l n e c n e n Somerset Pangnirtung EEZ Boundary a R M'Clure Strait h Island e C g Baffin Island Brodeur y e r r n Peninsula t a P I Cumberland n Peel Sound l e Sound Viscount Stefansson t Melville Island Sound Prince Labrador of Wales Igloolik Prince Sea it Island Charles ra Hadley Bay Banks St s Island le a Island W Hall Beach f Beaufort o M'Clintock Gulf of Iqaluit e c n Frobisher Bay i Channel Resolution r Boothia Boothia Sea P Island Sachs Franklin Peninsula Committee Foxe Harbour Strait Bay Melville Peninsula Basin Kimmirut Taloyoak N UNAT Minto Inlet Victoria SIA VUT Makkovik Ulukhaktok Kugaaruk Foxe Island Hopedale Liverpool Amundsen Victoria King -
Transits of the Northwest Passage to End of the 2016 Navigation Season Atlantic Ocean ↔ Arctic Ocean ↔ Pacific Ocean
TRANSITS OF THE NORTHWEST PASSAGE TO END OF THE 2016 NAVIGATION SEASON ATLANTIC OCEAN ↔ ARCTIC OCEAN ↔ PACIFIC OCEAN R. K. Headland revised 14 November 2016 Scott Polar Research Institute, University of Cambridge, Lensfield Road, Cambridge, United Kingdom, CB2 1ER. 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 255 complete maritime transits of the Northwest Passage have been made to the end of the 2016 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, from or to the Pacific Ocean (Bering Sea) through the Bering Strait. The Arctic Circle is crossed near the beginning and the end of all transits except those to or from the west coast of 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 154 and 171). These are shown on the map following, and proceed as follows: 1: Davis Strait, Lancaster Sound, Barrow Strait, Viscount Melville Sound, McClure Strait, Beaufort Sea, Chukchi Sea, Bering Strait. -
Pelagic Distribution Ol Seabirds-Western Lancaster Sound
Pelagic Distribution ol Seabirds-Western Lancaster Sound and Barro~ Strait Prelin1inary Report 1.977 ilj EMAR LIBRARY r.;r ,I l FISHERIES AND OCEANS CANADA TD 195 .P5 A35 1977 no.9 J 501 UNIVERSITY CRESCENT Nettleship, D.N. TD i Patterns of pelagic ! WINNIPEG, MB I' 17.r \ R3T 2N6 CANADA distribution of seabirds ... ~ .. I '"1: ·r.r J' ! .)~'f \ AIPP PRELIMINARY REPORT 1977 $5' ·._1) I )~1~ I Patterns of Pelagic Distribution of ·\ Seabirds in Western Lancaster Sound and no.c Barrow Strait, Northwest Territories, in "I August and September, 1976 D. N. Nettleship ~ l ..... A. J. Gaston I ~, I ! Canadian Wildlife Service Fisheries and Environment Canada Published under the Authority of the Hon. J. Hugh Faulkner Minister of Indian and Northern Affairs and the Hon. Len Marchand Minister of State (Environment) Ottawa, 1978 INA Publication No. QS-8160-009-EE-Al ESCOM Report No. AI-09 This report presents preliminary data and results obtained by Fisheries and Environment Canada for use by the Arctic Islands Pipeline Program. These investigations were carried out under the Environmental-Social Program, Northern Pipelines of the Government I) of Canada. While the studies and I. ', investigations were initiated to provide I I information necessary for the assessment ........ ": of hydrocarbon transportation proposals, the knowledge gained is equally useful in planning and assessing other development projects. Any opinions or conclusions expressed in this report are those of the authors and are not necessarily 'shared by the Government of Canada. , ' • 4 •• " I ,j :\ iii ·-> ;r RisuME .. I'; Nous avons etudie les caracteristiques de la repartition, de l'utilisation des habitats aquatiques et de l'aire d'alimenta tion des quatres especes principales d'ois_eaux de mer (le fulmar _boreal, fulmarus glaciatis, - la mouette tr idactyle, Rissa tridacty'la; la marm-ette de Br~nnich; Urici Comvia; et -le--guillemot noir, Cepphus qr11 Ue) qui se sont reproduites dans un terr itoire de 24 000 km2,~dans le detroit de Barrow et l'ouest du detroit de Lancaster, durant l'ete 1976. -
London Journal of Canadian Studies Article
London Journal of Canadian Studies Article Why Ross Survived When Franklin Died: Arctic Explorers and the Inuit, 1829–1848 Nicholas Bayne1,* How to cite: Bayne, N., ‘Why Ross Survived When Franklin Died: Arctic Explorers and the Inuit, 1829–1848’. London Journal of Canadian Studies, 2020, 35(1), pp. 67–95. DOI: https://doi.org/10.14324/111.444.ljcs.2020v35.004. Published: 30 November 2020 Peer Review: This article has been peer-reviewed through the journal’s standard double-blind peer review, where both the reviewers and authors are anonymized during review. Copyright: © 2020, Nicholas Bayne. This is an open-access article distributed under the terms of the Creative Commons Attribution Licence (CC-BY) 4.0 https://creativecommons.org/licenses/by/4.0/, which permits unrestricted use, distribution and reproduction in any medium, provided the original author and source are credited • DOI: https://doi.org/10.14324/111.444.ljcs.2020v35.004. Open Access: London Journal of Canadian Studies is a peer-reviewed open-access journal. * Correspondence: [email protected] 1 London School of Economic and Political Science, UK © 2020, Nicholas Bayne. This is an open-access article distributed under the terms of the Creative Commons Attribution Licence (CC-BY) 4.0 https://creativecommons.org/licenses/by/4.0/, which permits unrestricted use, distribution and reproduction in any medium, provided the original author and source are credited • DOI: https://doi.org/10.14324/111.444.ljcs.2020v35.004 Why Ross Survived When Franklin Died: Arctic Explorers and the Inuit, 1829–1848 Nicholas Bayne Abstract The Franklin expedition disappeared in the High Arctic in the 1840s, looking for the North-West Passage. -
Publications in Biological Oceanography, No
National Museums National Museum of Canada of Natural Sciences Ottawa 1971 Publications in Biological Oceanography, No. 3 The Marine Molluscs of Arctic Canada Elizabeth Macpherson CALIFORNIA OF SCIK NCCS ACADEMY |] JAH ' 7 1972 LIBRARY Publications en oceanographie biologique, no 3 Musees nationaux Musee national des du Canada Sciences naturelles 1. Belcher Islands 2. Evans Strait 3. Fisher Strait 4. Southampton Island 5. Roes Welcome Sound 6. Repulse Bay 7. Frozen Strait 8. Foxe Channel 9. Melville Peninsula 10. Frobisher Bay 11. Cumberland Sound 12. Fury and Hecia Strait 13. Boothia Peninsula 14. Prince Regent Inlet 15. Admiralty Inlet 16. Eclipse Sound 17. Lancaster Sound 18. Barrow Strait 19. Viscount Melville Sound 20. Wellington Channel 21. Penny Strait 22. Crozier Channel 23. Prince Patrick Island 24. Jones Sound 25. Borden Island 26. Wilkins Strait 27. Prince Gustaf Adolf Sea 28. Ellef Ringnes Island 29. Eureka Sound 30. Nansen Sound 31. Smith Sound 32. Kane Basin 33. Kennedy Channel 34. Hall Basin 35. Lincoln Sea 36. Chantrey Inlet 37. James Ross Strait 38. M'Clure Strait 39. Dease Strait 40. Melville Sound 41. Bathurst Inlet 42. Coronation Gulf 43. Dolphin and Union Strait 44. Darnley Bay 45. Prince of Wales Strait 46. Franklin Bay 47. Liverpool Bay 48. Mackenzie Bay 49. Herschel Island Map 1 Geographical Distribution of Recorded Specimens CANADA DEPARTMENT OF ENERGY, MINES AND RESOURCES CANADASURVEYS AND MAPPING BRANCH A. Southeast region C. North region B. Northeast region D. Northwest region Digitized by tlie Internet Archive in 2011 with funding from California Academy of Sciences Library http://www.archive.org/details/publicationsinbi31nati The Marine Molluscs of Arctic Canada Prosobranch Gastropods, Chitons and Scaphopods National Museum of Natural Sciences Musee national des sciences naturelles Publications in Biological Publications d'oceanographie Oceanography, No.