Holocene Climate And Environmental Change In The Palliser Triangle

The Palliser Triangle extends from south-west Manitoba to south central Alberta, and is one of the most climatically sensitive regions in Canada. There is evidence & concern that climate change is likely to affect the Triangle. The geological record contains unique information on the impacts of a wide range of past climate changes. This paleoenvironmental record, and the context it provides for assessing the impacts of future climate change, is the focus of the Palliser Triangle Global Change Project. This bulletin contains 18 papers related to two major objectives of that Project: reconstruction of Holocene climatic and hydrological changes, and evaluation of the relationships between climate & landscape processes. The first paper is an overview of the Project and a broad synthesis of major results. The next nine papers are devoted to records of past climate & hydrological change documented in paleolimnological and hydrogeological studies. The rest of the papers focus on geomorphic processes in the Triangle and how these respond to climate forcing.

The Palliser Triangle of south-west Saskatchewan and south-east Alberta is characterized by a variable climate, strong annual moisture deficit, and recurrent drought. Geomorphic systems in such environments are often sensitive to even minor changes in climate. This report considers four geomorphic systems in the Triangle (eolian, fluvial, mass wasting, and soil redistribution) and the ways they are likely to be affected by four climate change scenarios (warmer and drier, warmer and wetter, cooler and drier, and cooler and wetter), with the focus on the first scenario as being the most likely for the southern prairie region. The report begins with an overview of the Triangle's geological setting and its climate, vegetation, and soils. It then discusses the four geomorphic systems, and concludes with a qualitative discussion of the potential impacts of the climate change scenarios on each system and related human activities such as agriculture.

The Holocene spans the 11,500 years since the end of the last Ice Age and has been a period of major global environmental change. However the rate of change has accelerated during the last hundred years, due largely to human impacts and this has led to a growing concern for the future of our environmental resources. Global Change in the Holocene demonstrates how reconstructing the record of past environmental change can provide us with essential knowledge about how our environment works and presents the reader with an informed viewpoint from which to project realistic future scenarios. The book brings together key techniques that are widely used in Holocene research, such as radiocarbon dating, dendrochronology and sediment analysis and offers a comprehensive analysis of various archives of environmental change including instrumental and documentary records, corals, lake sediments, glaciers and ice cores. This reference will be an informative and cutting-edge resource for all researchers in the fields of climate change, environmental science, geography, palaeoecology and archaeology.

This book highlights climate as a complex physical, chemical, biological, and geological system, in perpetual change, under astronomical, predominantly, solar control. It has been shaped to some degree through the past glaciation cycles repeated in the last three million years. The Holocene, the current interglacial epoch which started ca. 11,700 years ago, marks the transition from the Stone Age to the unprecedented cultural evolution of our civilization. Significant climate changes have been recorded in natural archives during the Holocene, including the rapid waning of ice sheets, millennial shifting of the monsoonal fringe in the northern hemisphere, and abrupt centennial events. A typical case of severe environmental change is the greening of Sahara in the Early Holocene and the gradual desertification again since the fifth millennium before present. Climate Changes in the Holocene: Impact, Adaptation, and Resilience investigates the impact of natural climate changes on humans and civilization through case studies from various places, periods, and climates. Earth and human society are approached as a complex system, thereby emphasizing the necessity to improve adaptive capacity in view of the anthropogenic global warming and ecosystem degradation. Features: Written by distinguished experts, the book presents the fundamentals of the climate system, the unparalleled progress achieved in the last decade in the fields of intensified research for improved understanding of the carbon cycle, climate components, and their interaction. Presents the application of paleoclimatology and modeling in climate reconstruction. Examines the new era of satellite-based climate monitoring and the prospects of reduced carbon dioxide emissions.

Saskatchewan: Geographic Perspectives is Saskatchewan's first comprehensive geography textbook. Its major sections cover these themes: Physical Geography, Historical and Cultural Geography, Population and Settlement, and Economic Geography. Eighteen chapters provide an excellent overview of the province from a variety of geographic perspectives, while twenty-nine focus studies explore specific topics in depth ... presents the work of forty-three scholars and is well-illustrated, with more than 150 figures, 70 tables, and over 60 full-colour plates. It also includes full reference lists and a comprehensive index. Although prepared specifically for use in post-secondary geography programs, this book is also appropriate for high school research projects and for anyone interested in the many facets of this vast and varied province."--Googlebooks.

This is the only book to focus on the geomorphological landscapes of Canada West. It outlines the little-appreciated diversity of Canada’s landscapes, and the nature of the geomorphological landscape, which deserves wider publicity. Three of the most important geomorphological facts related to Canada are that 90% of its total area emerged from ice-sheet cover relatively recently, from a geological perspective; permafrost underlies 50% of its landmass and the country enjoys the benefits of having three oceans as its borders: the Arctic, Pacific and Atlantic oceans. Canada West is a land of extreme contrasts — from the rugged Cordillera to the wide open spaces of the Prairies; from the humid west-coast forests to the semi-desert in the interior of British Columbia and from the vast Mackenzie river system of the to small, steep, cascading streams on Vancouver Island. The thickest Canadian permafrost is found in the Yukon and extensive areas of the Cordillera are underlain by sporadic permafrost side-by-side with the never-glaciated plateaus of the Yukon. One of the curiosities of Canada West is the presence of volcanic landforms, extruded through the ice cover of the late Pleistocene and Holocene epochs, which have also left a strong imprint on the landscape. The Mackenzie and Fraser deltas provide the contrast of large river deltas, debouching respectively into the Arctic and Pacific oceans.

The Canadian Prairies in a Changing Climate is a comprehensive and up-to-date overview of climate change in the prairie provinces, the impacts on natural resources, communities, human health and sectors of the economy, and the adaptation options that are available for alleviating adverse impacts and taking advantage of new opportunities provided by a warmer climate.