By Hugh M. French, Olav Slaymaker
Chapter 1 chilly Canada and the altering Cryosphere (pages 1–25): Hugh French and Olav Slaymaker
Chapter 2 The overdue Quaternary Glaciation of Northern Canada (pages 26–47): David Evans
Chapter three The Evolution of Polar desolate tract and Tundra Ecosystems (pages 48–65): Konrad Gajewski
Chapter four distant Sensing and Canadian Snow Climatology (pages 66–86): Richard Kelly
Chapter five The altering Climates (pages 87–104): Roger Barry and Mark Serreze
Chapter 6 Snow and Runoff: strategies, Sensitivity and Vulnerability (pages 105–125): Ming?Ko Woo and John Pomeroy
Chapter 7 Permafrost Distribution and balance (pages 126–146): Chris Burn
Chapter eight Sea Ice in Canada (pages 147–162): David Barber and Jennifer Lukovich
Chapter nine Lake and River Ice in Canada (pages 163–181): Terry Prowse
Chapter 10 weather swap and the crucial Canadian Treeline (pages 183–199): Glen Macdonald
Chapter eleven Geomorphic switch in Northern Canada (pages 200–221): Hugh French
Chapter 12 Geomorphic swap in Canada's Temperate Mountains (pages 222–246): Olav Slaymaker
Chapter thirteen threat from Cold?climate dangers within the Canadian Cordillera (pages 247–266): Jim Gardner
Chapter 14 Societal elements of fixing chilly Environments (pages 267–300): Gita Laidler
Chapter 15 The altering Canadian Cryosphere, Globalization and international Environmental switch (pages 301–312): Olav Slaymaker and Hugh French
Read or Download Changing Cold Environments: A Canadian Perspective PDF
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Additional resources for Changing Cold Environments: A Canadian Perspective
This large river plays a vital role in the annual re-supply of settlements in the western Canadian Arctic. 2) constrain such activity, while annual flooding and periodic ice jams constitute hazards to bridges and settlements. On the other hand, in the broader catchment areas, frozen lakes and rivers are often the only means by which heavy construction equipment and other supplies are delivered to remote settlements and resource-exploitation sites in the winter months. 3 Cold Mountains The mountains of Canada represent the ‘alpine’ dimension of Canada’s cold environments.
Instead, the aim of this book is to simply document the changing nature of Canada’s cold environments and, by implication, outline the possible global impacts. We restrict the broader discussion to the northern hemisphere. Changing Cold Environments: A Canadian Perspective, First Edition. Edited by Hugh French and Olav Slaymaker. Ó 2012 John Wiley & Sons, Ltd. Published 2012 by John Wiley & Sons, Ltd. 1). Their relevance to climate change lies in: (i) their high surface reflectivity (albedo), (ii) the fact that all three phases of water (solid, liquid and vapour) coexist over the range of the Earth’s temperatures and pressures, and (iii) the large amount of latent heat associated with the phase changes between water and ice.
C. coast. The so-called Fluted Point people were hunters living close to the receding ice sheets $12–10 ka BP. Clearly, their lives must have been dominated by the cold environments into which they had moved. But by $4 ka BP the Early Nesikep culture of the BC Interior, the Early Northwest Coast culture and the Early Paleo-Eskimo cultures of the High Arctic and northwest Greenland had all emerged, and the environment had become quite similar to that of the present (Wright, 2001). As the ice sheets became more distant, life became progressively more influenced by the successive biomes that made eking out an existence so much more possible.