Nunavut Archaeology and Artifacts for Northern Heritage Workers Acknowledgments
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ARTH 315/CANS 315 Indigenous Art and Culture: Contemporary Indigenous Art in Canada Mcgill University, Montreal, Canada Fall 2020
ARTH 315/CANS 315 Indigenous Art and Culture: Contemporary Indigenous Art in Canada McGill University, Montreal, Canada Fall 2020 Lecture: Tuesday and Thursday, 1:05-1:50 pm, Arts W-215 (Lectures will be recorded on Zoom and posted after) Instructor: Dr. Gloria Bell Email: [email protected] Office Hours: Mondays 1:40 pm – 2:40pm. Tuesdays 2:30pm – 3:30 pm. Teaching Assistant: Rach Klein Email: tbd* Office Hours: (will be posted on MyCourses) Course Description: This course will examine the production of contemporary First Nations, Métis and Inuit artists in Canada from the 1990s to the present. A diverse range of contemporary art practices – including painting, drawing, photography, film, performance, installation and new media art – will be considered in relation to key aspects of the cultural, political and social life of Indigenous peoples in Canada. Much of the work examined reflects and responds to the continuing legacy of colonization and successive Canadian governments’ policies of assimilation and segregation. Artists, artworks and exhibitions examined will therefore be both historically and contemporarily contextualized. We will discuss the impact of the Indian Act, the establishment of Reserves and conflicts surrounding sovereignty and status, as well as the portrayal of Indigenous identity in art, popular culture and news media. Additionally, we will engage with the recent scholarship in Indigenous studies and material culture, and current events related to the theme of the course. The course is divided thematically, rather than chronologically, with weekly topics addressing significant aspects of Indigenous art and culture in Canada today. Objectives and Expectations: This course offers students the opportunity to critically engage with key themes in contemporary Indigenous art and culture. -
Contemporary Inuit Drawing
Cracking the Glass Ceiling: Contemporary Inuit Drawing Nancy Campbell A DISSERTATION SUBMITTED TO THE FACULTY OF GRADUATE STUDIES IN PARTIAL FULFILLMENT OF THE REQUIREMENTS FOR THE DEGREE OF DOCTOR OF PHILOSOPHY GRADUATE PROGRAM IN ART HISTORY, YORK UNIVERSITY TORONTO, ONTARIO. January 2017 © Nancy Campbell, 2017 Abstract The importance of the artist’s voice in art historical scholarship is essential as we emerge from post-colonial and feminist cultural theory and its impact on curation, art history, and visual culture. Inuit art has moved from its origins as an art representing an imaginary Canadian identity and a yearning for a romantic pristine North to a practice that presents Inuit identity in their new reality. This socially conscious contemporary work that touches on the environment, religion, pop culture, and alcoholism proves that Inuit artists can respond and are responding to the changing realities in the North. On the other side of the coin, the categories that have held Inuit art to its origins must be reconsidered and integrated into the categories of contemporary art, Indigenous or otherwise, in museums that consider work produced in the past twenty years to be contemporary as such. Holding Inuit artists to a not-so-distant past is limiting for the artists producing art today and locks them in a history that may or may not affect their work directly. This dissertation examines this critical shift in contemporary Inuit art, specifically drawing, over the past twenty years, known as the contemporary period. The second chapter is a review of the community of Kinngait and the role of the West Baffin Eskimo Cooperative in the dissemination of arts and crafts. -
A Spatial Evaluation of Arctic Sea Ice and Regional Limitations in CMIP6 Historical Simulations
1AUGUST 2021 W A T T S E T A L . 6399 A Spatial Evaluation of Arctic Sea Ice and Regional Limitations in CMIP6 Historical Simulations a a a a MATTHEW WATTS, WIESLAW MASLOWSKI, YOUNJOO J. LEE, JACLYN CLEMENT KINNEY, AND b ROBERT OSINSKI a Department of Oceanography, Naval Postgraduate School, Monterey, California b Institute of Oceanology of Polish Academy of Sciences, Sopot, Poland (Manuscript received 29 June 2020, in final form 28 April 2021) ABSTRACT: The Arctic sea ice response to a warming climate is assessed in a subset of models participating in phase 6 of the Coupled Model Intercomparison Project (CMIP6), using several metrics in comparison with satellite observations and results from the Pan-Arctic Ice Ocean Modeling and Assimilation System and the Regional Arctic System Model. Our study examines the historical representation of sea ice extent, volume, and thickness using spatial analysis metrics, such as the integrated ice edge error, Brier score, and spatial probability score. We find that the CMIP6 multimodel mean captures the mean annual cycle and 1979–2014 sea ice trends remarkably well. However, individual models experience a wide range of uncertainty in the spatial distribution of sea ice when compared against satellite measurements and reanalysis data. Our metrics expose common and individual regional model biases, which sea ice temporal analyses alone do not capture. We identify large ice edge and ice thickness errors in Arctic subregions, implying possible model specific limitations in or lack of representation of some key physical processes. We postulate that many of them could be related to the oceanic forcing, especially in the marginal and shelf seas, where seasonal sea ice changes are not adequately simulated. -
Thinking About the Arctic's Future
By Lawson W. Brigham ThinkingThinking aboutabout thethe Arctic’sArctic’s Future:Future: ScenariosScenarios forfor 20402040 MIKE DUNN / NOAA CLIMATE PROGRAM OFFICE, NABOS 2006 EXPEDITION The warming of the Arctic could These changes have profound con- ing in each of the four scenarios. mean more circumpolar sequences for the indigenous people, • Transportation systems, espe- for all Arctic species and ecosystems, cially increases in marine and air transportation and access for and for any anticipated economic access. the rest of the world—but also development. The Arctic is also un- • Resource development—for ex- an increased likelihood of derstood to be a large storehouse of ample, oil and gas, minerals, fish- yet-untapped natural resources, a eries, freshwater, and forestry. overexploited natural situation that is changing rapidly as • Indigenous Arctic peoples— resources and surges of exploration and development accel- their economic status and the im- environmental refugees. erate in places like the Russian pacts of change on their well-being. Arctic. • Regional environmental degra- The combination of these two ma- dation and environmental protection The Arctic is undergoing an jor forces—intense climate change schemes. extraordinary transformation early and increasing natural-resource de- • The Arctic Council and other co- in the twenty-first century—a trans- velopment—can transform this once- operative arrangements of the Arctic formation that will have global im- remote area into a new region of im- states and those of the regional and pacts. Temperatures in the Arctic are portance to the global economy. To local governments. rising at unprecedented rates and evaluate the potential impacts of • Overall geopolitical issues fac- are likely to continue increasing such rapid changes, we turn to the ing the region, such as the Law of throughout the century. -
Inuit Art & Culture Tours
Inuit Art & Culture Tours A Teacher’s Guide Dear Teacher, Thank you for participating in an Inuit Cultural Tour or the Inuit Partnership Program at the Dennos Museum Center. We are excited to see you and your students at the museum soon! This packet gives you some background on the Inuit people and outlines the goals of the Inuit Cultural Tours. Specific details of the tour (length of tour, art project, etc.) will vary with each group. Please refer to your tour confirmation sheet to verify specific details of your tour. There are three suggested pre- or post-activities and a list of possible lesson extensions included in the packet. Please use and alter any of these lessons as you wish to create an integrated unit of study and complete the museum learning experience for your students. If your class is participating in the printmaking activity during your museum visit, please make sure that the students prepare their sketches on the worksheet provided outside of this packet. There is also an evaluation included in your materials. Please fill it out and return it to the museum. Your feedback on the packet and tour experience is vital for planning future programming! Thank you, Jason Dake Curator of Education (231) 995-1029 [email protected] 2 INUIT CULTURAL TOURS TOUR OVERVIEW This tour program is built around the Dennos Museum Center’s collection of Inuit Art and Michigan State Social Studies and Art Curriculum standards. Combined with the included lessons, this program also addresses curriculum standards for English/Language Arts. It combines art production, hands-on learning, games, and aesthetics to engage students with the Inuit people. -
Discover Inuit
) DiscoverDiscover InuitInuit ArtArt What do polar bears look like when they stand up on their hind legs? What kinds of creatures are the heroes of Inuit legends? How did Inuit mothers keep their babies warm through the freezing arctic days and nights? What does an Inuit summer camp look like? What are some of the big concerns for young Inuit today? You’ll learn the answers) to all these questions, and The detail in Inuit sculpture hundreds more, through and colourful drawings will open more doors than you can imagine. the wonderful world Many of the older Inuit artists working today grew up in a traditional way. They of Inuit art. lived in igloos in winter and tents made of animal skins in summer. Their families returned to their winter and summer camps each year when the sea mammals and animals (like seals, whales and caribou), came in greatest numbers. Mothers carried their babies in an amauti — the big hood on their parkas. When the family travelled, it was on a sled pulled by a dog team. What Inuit art shows This traditional way of life is one of the big subjects in Inuit art. By showing us in drawings and sculptures how their ancestors lived, Inuit artists are keeping their history alive. Art helps them remember, and treasure, the ways their ancestors hunted and made protective clothing and shelter. In their Stories of ) art, many Inuit are making a visual history to show how their ancestors adapted to living in one of the harshest climates shamans tell on earth. -
Some Aspects of the Thermal Energy Exchange on the South Polar Snow Field and Arctic Ice Pack'
MAY 1961 MONTHLY WEATHER REVIEW 173 SOME ASPECTS OF THE THERMAL ENERGY EXCHANGE ON THE SOUTH POLAR SNOW FIELD AND ARCTIC ICE PACK' KIRBY J. HANSON Po!ar Meteorology Research Project, US. Weather Bureau, Washington, D.C. [Manuscript received September 13, 1960; revised February 21, 1961 ] ABSTRACT Solar and terrestrial radiation measurements that were obtained at Amundsen-Scot>t (South Pole) Station and on Ice lsland (Bravo) T-3 are presented for representative summer and winter months. Of the South Polar net radiation loss during April 1958, approximately20 percent of the energy came from the snow and80 percent from the air. The actual atmospheric cooling rate during that period was only about lj6 of the suggested radiative cooling rate. The annual net radiation at various places in Antarctica is presented. During 1058, the South Polar atmos- phere transmitted about 73 percent of the annual extraterrestrial radiation, while at T-3 the Arctic atmosphere transmitted about 56 percent. The albedo of melting sea ice is discussed. Measurements on T-3 during July 1958 indicate that the net radiation is positive on both clear and overcast days but greatest on overcast days. Refreezing of the surface with clear skies, as observed by Untersteiner and Badglep, is discussed. 1. INTRODUCTION Ocean.ThisIsland wasabout by 5 11 miles in size and The elliptical orbit of the earthbrings it about 3 million about 52 meters thick (Crary et al. [2]) in 1953 when it miles farther from the sun at aphelion than at perihelion; drifted near 88' N., looo W. In the years that followed, consequently,during midsummer, about 7 percent less this it drifted southward and in July 1958 was located solar radiation impinges on the top of the Arctic atrnos- 79.5' N., 118' W. -
Downloaded 10/01/21 10:31 PM UTC 874 JOURNAL of CLIMATE VOLUME 12
MARCH 1999 VAVRUS 873 The Response of the Coupled Arctic Sea Ice±Atmosphere System to Orbital Forcing and Ice Motion at 6 kyr and 115 kyr BP STEPHEN J. VAVRUS Center for Climatic Research, Institute for Environmental Studies, University of WisconsinÐMadison, Madison, Wisconsin (Manuscript received 2 February 1998, in ®nal form 11 May 1998) ABSTRACT A coupled atmosphere±mixed layer ocean GCM (GENESIS2) is forced with altered orbital boundary conditions for paleoclimates warmer than modern (6 kyr BP) and colder than modern (115 kyr BP) in the high-latitude Northern Hemisphere. A pair of experiments is run for each paleoclimate, one with sea-ice dynamics and one without, to determine the climatic effect of ice motion and to estimate the climatic changes at these times. At 6 kyr BP the central Arctic ice pack thins by about 0.5 m and the atmosphere warms by 0.7 K in the experiment with dynamic ice. At 115 kyr BP the central Arctic sea ice in the dynamical version thickens by 2±3 m, accompanied bya2Kcooling. The magnitude of these mean-annual simulated changes is smaller than that implied by paleoenvironmental evidence, suggesting that changes in other earth system components are needed to produce realistic simulations. Contrary to previous simulations without atmospheric feedbacks, the sign of the dynamic sea-ice feedback is complicated and depends on the region, the climatic variable, and the sign of the forcing perturbation. Within the central Arctic, sea-ice motion signi®cantly reduces the amount of ice thickening at 115 kyr BP and thinning at 6 kyr BP, thus serving as a strong negative feedback in both pairs of simulations. -
Development in the Arctic
Take ourWin reader a WWF survey: Arctic panda.org/thecircle gift pack! MAGAZINE Working together 9 No. 1 A wave of investment 16 2018 THE CIRCLE Energy in a changing north 20 WHAT’S NEXT FOR THE ARCTIC? PUBLISHED BY THE WWF ARCTIC PROGRAMME THE CIRCLE 1.2018 WHAT’S NEXT FOR THE ARCTIC? Contents EDITORIAL Change: the big picture 3 IN BRIEF 4 JANET PAWLAK Snow, water, ice and permafrost 6 CINDY DICKSON Working together 9 EMILY MCKENZIE and KATHERINE WYATT Connections with nature 10 JAMES E. PASS Development in the Arctic 12 KATHARINA SCHNEIDER-ROOS and LORENA ZEMP Sustain- able and resilient infrastructure 14 ALAN ATKISSON A wave of investment 16 OKALIK EEGEESIAK Inuit and the Ice Blue Economy 18 NILS ANDREASSEN Energy in a changing North 20 SVEIN VIGELAND ROTTEM The Arctic Council – a need for reform 21 TOM BARRY and COURTNEY PRICE Arctic biodiversity: challenges 22 The contest 24 The Circle is published quarterly Publisher: Editor in Chief: Leanne Clare, COVER: Snow mobile travel over by the WWF Arctic Programme. WWF Arctic Programme [email protected] sea ice in Uummannaq, Green- Reproduction and quotation with 8th floor, 275 Slater St., Ottawa, land appropriate credit are encour- ON, Canada K1P 5H9. Managing Editor: Becky Rynor, Photo: Lawrence Hislop, www.grida.no/resources/1151 aged. Articles by non-affiliated Tel: +1 613-232-8706 [email protected] sources do not necessarily reflect Fax: +1 613-232-4181 ABOVE: Boy on bicycle, Nuuk, the views or policies of WWF. Design and production: Send change of address and sub- Internet: www.panda.org/arctic Film & Form/Ketill Berger, Greenland. -
Educator Guide
E DUCATOR GUIDE This guide, and its contents, are Copyrighted and are the sole Intellectual Property of Science North. E DUCATOR GUIDE The Arctic has always been a place of mystery, myth and fascination. The Inuit and their predecessors adapted and thrived for thousands of years in what is arguably the harshest environment on earth. Today, the Arctic is the focus of intense research. Instead of seeking to conquer the north, scientist pioneers are searching for answers to some troubling questions about the impacts of human activities around the world on this fragile and largely uninhabited frontier. The giant screen film, Wonders of the Arctic, centers on our ongoing mission to explore and come to terms with the Arctic, and the compelling stories of our many forays into this captivating place will be interwoven to create a unifying message about the state of the Arctic today. Underlying all these tales is the crucial role that ice plays in the northern environment and the changes that are quickly overtaking the people and animals who have adapted to this land of ice and snow. This Education Guide to the Wonders of the Arctic film is a tool for educators to explore the many fascinating aspects of the Arctic. This guide provides background information on Arctic geography, wildlife and the ice, descriptions of participatory activities, as well as references and other resources. The guide may be used to prepare the students for the film, as a follow up to the viewing, or to simply stimulate exploration of themes not covered within the film. -
International Dimensions
CHAPTER 9 International Dimensions NATIONAL ISSUES REPORT NATIONAL ISSUES REPORT 624 Coordinating lead author Jimena Eyzaguirre, ESSA Technologies Ltd. Lead authors Cedar Morton, PhD, ESSA Technologies Ltd. Colette Wabnitz, PhD, University of British Columbia and Stanford University Michael Copage, Environment and Climate Change Canada Robert McLeman, PhD, Wilfrid Laurier University Contributing authors Danica Lassaline, Environment and Climate Change Canada Juliano Palacios-Abrantes, PhD, University of British Columbia Kamleshan Pillay, PhD,, Independent Adaptation Finance Specialist Recommended citation Eyzaguirre, J., Morton, C., Wabnitz, C., Copage, M. and McLeman, R. (2021): International Dimensions; Chapter 9 in Canada in a Changing Climate: National Issues Report, (ed.) F.J. Warren and N. Lulham; Government of Canada, Ottawa, Ontario. NATIONAL ISSUES REPORT 625 Table of contents Key messages 627 9.1 Introduction 628 9.1.1 Overview of findings from past assessments 630 9.2 Climate change affects Arctic shipping and threatens sovereignty 631 9.2.1 Introduction 631 9.2.2 Climate, sea ice and Arctic navigation 631 9.2.3 Climate-related risks to Canada’s control over the Northwest Passage 637 9.2.4 Strategies to adapt to increased shipping activity in the Northwest Passage 640 Case Story 9.1: Adaptation strategies for cruise ship tourism in the Canadian Arctic 643 9.3 Transboundary marine and freshwater agreements generally do not consider climate change 644 9.3.1 Introduction 645 Case Story 9.2: The Canada–U.S. Pacific Salmon Treaty 646 9.3.2 Marine agreements 648 9.3.3 Freshwater agreements 652 Case Story 9.3: Modernizing the Canada–U.S. -
From Alaska to Greenland: a Comparison of the Arctic Small Tool
microblades, burins and burin spalls, and projectile points and scrapers that resemble those From Alaska to Greenland: A recovered from settlements around Lake Baikal Comparison of the Arctic Small Tool and elsewhere in eastern Siberia (McGhee 1996; Nash 1969). Charcoal found in Feature 17 at the and Thule Traditions Kuzitrin Lake Denbigh site in Alaska has produced radiocarbon dates ranging from 5500 to 4000 B.P.(Harritt 1998:63-69). Harritt (1998) states that the earliest known Denbigh material could possibly signify the appearance of the In this paper, I will discuss the Denbigh culture from Siberia in western Alaska. distinguishing cultural characteristics of the Within this west to east migration Arctic Small Tool tradition (ASTt) and Thule model, two major ASTt variants have been tradition, and hypothesize about the implications identified in the High Arctic: Independence I and that these characteristics have on the Pre-Dorset. Charcoal from Independence I sites understanding of the ASTt and Thule ways of have provided a radiocarbon date range from life. The ASTt and Thule migrations occurred about 4000 to 3700 B.P. These sites are located approximately 3000 years apart from each other. in Greenland, and on the High Arctic of Canada They represent in the archaeological record two at Devon, Cornwallis, and Ellesmere Islands. rapid, widespread migrations across the Arctic Independence I sites also likely occur in the Low from the western coasts of Alaska to those of Arctic, however they are hard to recognize due to eastern Greenland. The material culture left the small size of camps and the amount of tundra behind by these peoples clearly indicates two vegetation that may be covering them (McGhee very different lifestyles and adaptations to the 1978:30).