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G3292 WESTERN HEMISPHERE. REGIONS, NATURAL G3292 FEATURES, ETC. .D3 Darien Gap Highway [Colombia and Panama] .L3 Latin America .N4 New Spain 14 G3302 NORTH AMERICA. REGIONS, NATURAL FEATURES, G3302 ETC. .A4 Alaska Highway .C6 Coasts .I5 Inside Passage .W5 Winnipeg, Lake, Watershed 15 G3312 GREAT LAKES AGGREGATION. REGIONS, NATURAL G3312 FEATURES, ETC. .D4 Detroit River [MI & Ont.] .E7 Erie, Lake .H8 Huron, Lake [MI & Ont.] .M3 MacKinac, Straits of .M5 Michigan, Lake .N5 Niagara Falls [NY & Ont.] .N52 Niagara River [NY & Ont.] .O5 Ontario, Lake [NY & Ont.] .S43 Saint Clair, Lake [MI & Ont.] .S44 Saint Clair River [MI & Ont.] .S5 Saint Lawrence River .S53 Saint Lawrence Seaway .S55 Saint Marys River [MI & Ont.] .S9 Superior, Lake .T5 Thousand Islands [NY & Ont.] 16 G3382 GREENLAND. REGIONS, NATURAL FEATURES, ETC. G3382 .C7 Crownprince Christian Land .D3 Daugaard-Jensen Land .D5 Disko Bay .D53 Disko Island .H2 Hall Basin [Greenland & Nunavut] .H25 Hall Land .H3 Hayes Peninsula .H6 Hochstetter Forland .I4 Ilimaussaq Mountain .I5 Inglefield Gulf .J3 Jameson Land .K2 Kane Basin [Greenland & Nunavut] .K3 Kangerlussuaq .K35 Kennedy Channel [Greenland & Nunavut] .K4 King Christian IX Land .K45 King Christian X Land .K5 King Frederik IX Land .K55 King Frederik VI Coast .K6 King Frederik VIII Land .M4 Melville Bay .M5 Milne Land .N2 Nares Strait [Greenland & Nunavut] .N3 Nationalparken .N6 North Star Bay .N8 Nugssuaq Island .N83 Ngssuaq Peninsula .P4 Peary Land .R6 Robeson Channel .S3 Scoresby Land .S5 Skaergården Channel .S6 Skovfjorden (Fjord) .S7 Smith Sound [Greenland & Nunavut] .S8 Stosch Cape .S9 Svartenhuk Peninsula .U2 Ubekendt Island .U8 Uummannaq Fjord .W3 Washington Land .W4 Werner Mountain 17 G3384 GREENLAND. CITIES AND TOWNS, ETC. G3384 .A5 Angmagssalik .C5 Christianshaab .D8 Dundas .E5 Egedesminde .I4 Iluissat .J9 Julianehaab .K3 Kangatsiak .N3 Nanortalik .N35 Narssak .N36 Narssaq .N8 Nuuk .P3 Paamiut .Q15 Qaanaaq .Q2 Qeqertarsuaq .S3 Scoresbysund .S5 Sisimiut .S9 Sukkertoppen .U5 Umanak .U6 Upernavik 18 .

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Of Penguins and Polar Bears Shapero Rare Books 93
OF PENGUINS AND POLAR BEARS Shapero Rare Books 93 OF PENGUINS AND POLAR BEARS EXPLORATION AT THE ENDS OF THE EARTH 32 Saint George Street London W1S 2EA +44 20 7493 0876 [email protected] shapero.com CONTENTS Antarctica 03 The Arctic 43 2 Shapero Rare Books ANTARCTIca Shapero Rare Books 3 1. AMUNDSEN, ROALD. The South Pole. An account of “Amundsen’s legendary dash to the Pole, which he reached the Norwegian Antarctic Expedition in the “Fram”, 1910-1912. before Scott’s ill-fated expedition by over a month. His John Murray, London, 1912. success over Scott was due to his highly disciplined dogsled teams, more accomplished skiers, a shorter distance to the A CORNERSTONE OF ANTARCTIC EXPLORATION; THE ACCOUNT OF THE Pole, better clothing and equipment, well planned supply FIRST EXPEDITION TO REACH THE SOUTH POLE. depots on the way, fortunate weather, and a modicum of luck”(Books on Ice). A handsomely produced book containing ten full-page photographic images not found in the Norwegian original, First English edition. 2 volumes, 8vo., xxxv, [i], 392; x, 449pp., 3 folding maps, folding plan, 138 photographic illustrations on 103 plates, original maroon and all full-page images being reproduced to a higher cloth gilt, vignettes to upper covers, top edges gilt, others uncut, usual fading standard. to spine flags, an excellent fresh example. Taurus 71; Rosove 9.A1; Books on Ice 7.1. £3,750 [ref: 96754] 4 Shapero Rare Books 2. [BELGIAN ANTARCTIC EXPEDITION]. Grande 3. BELLINGSHAUSEN, FABIAN G. VON. The Voyage of Fete Venitienne au Parc de 6 a 11 heurs du soir en faveur de Captain Bellingshausen to the Antarctic Seas 1819-1821.
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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.
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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.
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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.
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Thermodynamic and Dynamic Ice Thickness Contributions in the Canadian Arctic Archipelago in NEMO-LIM2 Numerical Simulations
The Cryosphere, 12, 1233–1247, 2018 https://doi.org/10.5194/tc-12-1233-2018 © Author(s) 2018. This work is distributed under the Creative Commons Attribution 4.0 License. Thermodynamic and dynamic ice thickness contributions in the Canadian Arctic Archipelago in NEMO-LIM2 numerical simulations Xianmin Hu1,a, Jingfan Sun1,b, Ting On Chan1,c, and Paul G. Myers1 1Department of Earth and Atmospheric Sciences, University of Alberta, Edmonton, T6G 2E3, Canada anow at: Bedford Institute of Oceanography, Fisheries and Oceans Canada, Dartmouth, Nova Scotia, Canada bnow at: School of Electrical and Computer Engineering, Georgia Institute of Technology, Atlanta, GA, USA cnow at: Skytech Solutions Ltd., Canada Correspondence: Xianmin Hu ([email protected]) Received: 6 September 2017 – Discussion started: 10 October 2017 Revised: 16 March 2018 – Accepted: 19 March 2018 – Published: 10 April 2018 Abstract. Sea ice thickness evolution within the Canadian is found in the northern CAA and Bafﬁn Bay while a de- Arctic Archipelago (CAA) is of great interest to science, as cline (r2 ≈ 0:6, p < 0:01) is simulated in Parry Channel re- well as local communities and their economy. In this study, gion. The two main contributors (thermodynamic growth and based on the NEMO numerical framework including the lateral transport) have high interannual variabilities which LIM2 sea ice module, simulations at both 1=4 and 1=12◦ hor- largely balance each other, so that maximum ice volume can izontal resolution were conducted from 2002 to 2016. The vary interannually by ±12 % in the northern CAA, ±15 % in model captures well the general spatial distribution of ice Parry Channel, and ±9 % in Bafﬁn Bay.
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ARCTIC Exploration the SEARCH for FRANKLIN
CATALOGUE THREE HUNDRED TWENTY-EIGHT ARCTIC EXPLORATION & THE SeaRCH FOR FRANKLIN WILLIAM REESE COMPANY 409 Temple Street New Haven, CT 06511 (203) 789-8081 A Note This catalogue is devoted to Arctic exploration, the search for the Northwest Passage, and the later search for Sir John Franklin. It features many volumes from a distinguished private collection recently purchased by us, and only a few of the items here have appeared in previous catalogues. Notable works are the famous Drage account of 1749, many of the works of naturalist/explorer Sir John Richardson, many of the accounts of Franklin search expeditions from the 1850s, a lovely set of Parry’s voyages, a large number of the Admiralty “Blue Books” related to the search for Franklin, and many other classic narratives. This is one of 75 copies of this catalogue specially printed in color. Available on request or via our website are our recent catalogues: 320 Manuscripts & Archives, 322 Forty Years a Bookseller, 323 For Readers of All Ages: Recent Acquisitions in Americana, 324 American Military History, 326 Travellers & the American Scene, and 327 World Travel & Voyages; Bulletins 36 American Views & Cartography, 37 Flat: Single Sig- nificant Sheets, 38 Images of the American West, and 39 Manuscripts; e-lists (only available on our website) The Annex Flat Files: An Illustrated Americana Miscellany, Here a Map, There a Map, Everywhere a Map..., and Original Works of Art, and many more topical lists. Some of our catalogues, as well as some recent topical lists, are now posted on the internet at www.reeseco.com.
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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.
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Fall Ice Drift in Nares Strait, As Observed by Sideways-Looking
ARCTIC VOL. 32. NO. 4 (DEC. 1979). P. 283-307 Fall Ice Drift in Nares Strait, as Observedby Sideways-Looking Airborne Radar MOIRA DUNBAR’ ABSTRACT. From Sideways-Looking Airborne Radar (SLAR) imagery of sea ice obtained on three flights during the week of 19 to 26 Oct. 1976 it is possible to track floes throughout Nares Strait over periods of days and, on one occasion, hours. The dataare interpreted in the lightof available information on ice drift, winds, and currents. The results are believed to give a fairly typical picture of ice drift characteristics in periods of northerly air flow, which is the dominant pattern in this area. The suitability of the method for acquiring drift information in other areas is also demonstrated. RfiSUMk Des clichés SLAR de glace de mer, pris lors de trois vols, pendant la semaine du 19 au 26 octobre 1976, permettaient de suivre de près des glaces flottantes dans la détroit de Nares pendant des jours et des heures à une occasion. Certainement les résultats donnent une image typique correcte des proprietts de la dérive des glaces pendant les périodes où le vent du Nord souffle, ce qui est le cas génèralement dans cette région. C’était un bon exemple de crtdibilité de la mbthode à appliquer dans l’autres régions pour acquérir de l’information sur la dèrive des glaces. Traduit par Alain de Vendegies, Aquitaine Co. of Canada Ltd. INTRODUCTION The imagery on which this study is based was obtained by a Canadian Forces Argus aircraft as part of a joint CanadianlUK exercise designed primarily to provide top and bottom profiles of ice in the Arctic Ocean.
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Spatial Variation in Arctic Hare (Lepus Arcticus) Populations Around the Hall Basin
Spatial variation in Arctic hare (Lepus arcticus) populations around the Hall Basin Fredrik Dalerum1,2,3, Love Dalén2,4, Christina Fröjd5, Nicolas Lecomte6, Åsa Lindgren5, Tomas Meijer2,7, Patricia Pecnerova2,4, Anders Angerbjörn2 1 Research Unit of Biodiversity, Department of Biology of Organisms and Systems, University of Oviedo, Spain 2 Department of Zoology, Stockholm University, Sweden 3 Mammal Research Institute, Department of Zoology, University of Pretoria, South Africa 4 Department of Bioinformatics and Genetics, Swedish Museum of Natural History, Sweden 5 Swedish Polar Research Secretariat, Sweden 6 Canada Research Chair in Polar and Boreal Ecology and Centre d’Études Nordiques, Department of Biology, University of Moncton, Canada 7 Section for Wildlife Diseases, Swedish National Veterinary Institute, Travvägen 12A, 756 51 Uppsala, Sweden Published in Polar Biology, October 2017, Volume 40, Issue 10, pp 2113–2118 1 Abstract Arctic environments have relatively simple ecosystems. Yet, we still lack knowledge of the spatio- temporal dynamics of many Arctic organisms and how they are affected by local and regional processes. The Arctic hare (Lepus arcticus) is a large lagomorph endemic to high Arctic environments in Canada and Greenland. Current knowledge about this herbivore is scarce and the temporal and spatial dynamics of their populations are poorly understood. Here we present observations on Arctic hares in two sites on north Greenland (Hall and Washington lands) and one adjacent site on Ellesmere Island (Judge Daly Promontory). We recorded a large range of group sizes from 1 to 135 individuals, as well as a substantial variation in hare densities among the three sites (Hall land: 0 animals / 100 km2, Washington land 14.5-186.7 animals / 100 km2, Judge Daly Promontory 0.18-2.95 animals / 100 km2).
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ARCTIC VOL. 71, NO. 3 (SEPTEMBER 2018) P. 334 – 348 https://doi.org/10.14430/arctic4735 Seal Occurrence and Habitat Use during Summer in Petermann Fjord, Northwestern Greenland Kate Lomac-MacNair,1,2 Martin Jakobsson,3 Alan Mix,4 Francis Freire,3 Kelly Hogan,5 Larry Mayer6 and Mari A. Smultea2 (Received 29 June 2017; accepted in revised form 30 May 2018) ABSTRACT. Ice-associated seals are considered especially susceptible and are potentially the first to modify distribution and habitat use in response to physical changes associated with the changing climate. Petermann Glacier, part of a unique ice-tongue fjord environment in a rarely studied region of northwestern Greenland, lost substantial sections of its ice tongue during major 2010 and 2012 calving events. As a result, changes in seal habitat may have occurred. Seal occurrence and distribution data were collected in Petermann Fjord and adjacent Nares Strait region over 27 days (2 to 28 August) during the multidisciplinary scientific Petermann 2015 Expedition on the icebreaker Oden. During 239.4 hours of dedicated observation effort, a total of 312 individuals were recorded, representing four species: bearded seal (Erignathus barbatus), hooded seal (Crystophora cristata), harp seal (Pagophilus groenlandicus), and ringed seal (Pusa hispida). Ringed seals were recorded significantly more than the other species (χ2 = 347.4, df = 3, p < 0.001, n = 307). We found significant differences between species in haul-out (resting on ice) behavior (χ2 = 133.1, df = 3, p < 0.001, n = 307). Bearded seals were more frequently hauled out (73.1% n = 49), whereas ringed seals were almost exclusively in water (93.9%, n = 200).
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September 2009 Regional Sea Ice Outlooks: July Report Community
September 2009 Regional Sea Ice Outlooks: July Report Community Contributions 1 Table of Contents Hajo Eicken, Chris Petrich, and Mette Kaufman 3–6 Oleg Pokrovsky 7–9 Don Perovich 10 Charles Fowler, Sheldon Drobot, and James Maslanik 11–15 Jinlun Zhang 16–17 Preben Gudmandsen, Ron Kwok, Andreas Muenchow, Roger Samelson, and Jeremy Wilkinson 18–20 Stephen Howell and Claude Duguay 21–22 Sebastian Gerland and Harvey Goodwin 23–26 2 September 2009 Regional Sea Ice Outlook: July Report A regional perspective on ice evolution in the Pacific Arctic sector (SIZONet project) Submitted By: Hajo Eicken, Chris Petrich, and Mette Kaufman on behalf of the Seasonal Ice Zone Observing Network (SIZONet) Contact information Hajo Eicken: [email protected] Chris Petrich: [email protected] Mette Kaufman: [email protected] SIZONet: http://www.sizonet.org With support from the National Science Foundation’s Arctic Observing Network Program and the Alaska Ocean Observing System. (1) Region of interest: Bering-Chukchi-Beaufort Seas (2) Ice development and status in early July 2009 Ice extent: • Passive microwave data (SSM/I) distributed by the National Snow and Ice Data Center (NSIDC) indicate above-normal ice extent in the Bering Sea for April 2009 (Figure 1). Starting in early May, vigorous and early melt resulted in rapid northward retreat of the ice edge to below normal extent in June and early July (Figure 2). Ice thickness and ice characteristics: • Eastern Chukchi/Western Beaufort Sea: End-of-winter ice thickness distribution as presented in our June Report, i.e., much less multiyear ice of thickness comparable to previous years (3.6 m total level ice thickness mode) and first-year ice thicknesses comparable to or thicker than past years (1.7 m total level ice thickness mode with thicker deformed ice).
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Ice Regime and Ice Transport in Nares Strait
Ice Regime and Ice Transport in Nares Strait MOIRA DUNBAR1 ABSTRACT. In order to assess the part played by ice export through the Canadian Arctic Archipelago in the heat budget of the Arctic Ocean, one of the factors that must be known is the length of time per year that the channels are sealed by fast ice. To establish this for Nares Strait a series of flights was undertaken through the winters of 1970-71 and 1971-72. The resulting observations, combined with a search of historical records, suggest that the dateof consolidation of ice in this channel tends to be late. A tentative calculation of annual export leads to the conclusion that the contribution of the Canadian channels may be greater than has been supposed. RfiSUMe. Rdgime et transport des glacesdans le ddtroit de Nares.Pour Bvaluer la part que jouel’exportation des glaces51 travers les chenaux arctiques dans lebilan thermique de l’océan Arctique, l‘un des facteurs qu’il faut connaître est la longueur de la pBriode annuelle pendantlaquelle les chenaux sont bloquBs par la glace fixBe. Pour le constater dans le d6troit de Nares, nous avons entrepris une sBrie d‘envolks pendant les hivers de 1970-1971 et 1971-1972. Nos observations, jointes à une recherche de données historiques, nous suggèrent que la datede consolidation de la glace dans ce chenal tend B être tardive. Un essai de calcul de l’exportation annuelle nous amène 51 conclure que la contribution des chenaux canadienspourrait êtreplus grande qu’on ne l’avait supposé. INTRODUCTION Estimates of ice transport out of the Arctic Ocean are quite varied, which is not surprising in view of the fact that they are based on a number of other factors, all of which are imperfectly known.
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