This book gives an overview of the state of research in fields pertaining to the detection, understanding and prediction of global change impacts in mountain regions. More than sixty contributions from paleoclimatology, cryospheric research, hydrology, ecology, and development studies are compiled in this volume, each with an outlook on future research directions. The book will interest meteorologists, geologists, botanists and climatologists.

Mountain regions encompass nearly 24 percent of the total land surface of the earth and are home to approximately 12 percent of the world's population. Their ecosystems play a critical role in sustaining human life both in the highlands and the lowlands. During recent years, resource use in high mountain areas has changed mainly in response to the

This book is written for general readers with an interest in science, and offers the tools and ideas for understanding how climate change will affect mountains of the American West. A major goal of the book is to provide material that will not become quickly outdated, and it does so by conveying its topics through constants in ecological science that will remain unchanged and scientifically sound. The book is timely in its potential to be a long-term contribution, and is designed to inform the public about climate change in mountains accessibly and intelligibly. The major themes of the book include: 1) mountains of the American West as natural experiments that can distinguish the effects of climate change because they have been relatively free from human-caused changes, 2) mountains as regions with unique sensitivities that may change more rapidly than the Earth as a whole and foreshadow the nature and magnitude of change elsewhere, and 3) different interacting components of ecosystems in the face of a changing climate, including forest growth and mortality, ecological disturbance, and mountain hydrology. Readers will learn how these changes and interactions in mountains illuminate the complexity of ecological changes in other contexts around the world.

Glaciers in the Andes are particularly important natural archives of present and past climatic and environmental changes, in significant part because of the N-S trend of this topographic barrier and its influence on the atmospheric circulation of the southern hemisphere. Strong gradients in the seasonality and amount of precipitation exist between the equator and 30° S. Large differences in amount east and west of the Andean divide also occur, as well as a change from tropical summer precipitation (additionally modified by the seasonal shift of the circulation belts) to winter precipitation in the west wind belt (e. g. , Yuille, 1999; Garraud and Aceituno, 2001). The so-called 'dry axis' lies between the tropical and extra tropical precipitation regimes (Figure 1). The high mountain desert within this axis responds most sensitively to the smallest changes in effective moisture. An important hydro-meteorological feature on a seasonal to inter-annual time-scale is the occurrence of EN SO events, which strongly control the mass balance of glaciers in this area (e. g. , Wagnon et ai. , 2001; Francou et ai. , in press). The precipitation pattern is an important factor for the interpretation of climatic and environmental records extracted from ice cores, because much of this information is related to conditions at the actual time of precipitation, and this is especially so for stable isotope records. Several ice cores have recently been drilled to bedrock in this area. From Huascanin (Thompson et ai. , 1995), Sajama (Thompson et ai.

This second edition of the book Sustainable Development of Mountain Regions: Southeastern Europe integrates the scientific results and expertise of the researchers from the countries in Southeastern Europe. The book consists of updated information for the topics observed in first edition and several new chapters with analysis of some problems in the mountain regions of four new for the edition countries in Southeastern European space. The general themes in the book are related to Global problems and mountain regions; Nature resources and landuse in mountain regions; Social, economic and regional problems of mountain regions; Nature protection, conservation and monitoring and Networks and strategies for mountain regions. The key topics for discussion are: Natural recourses and land use in mountain regions. Sustainable social and economic development of the mountain regions. Natural disasters and risk prevention. Spatial modeling and planning. Nature protection, monitoring and conservation. Politics and sustainable practices for development of mountain regions. Transborder and regional cooperation. Mountain regions in Southeastern Europe are characterized by unique landscape and biological diversity and great economic potential. They have function as a living space and provide different groups of ecosystem and landscape services. In social and economic aspects these regions are one of the poorest in Southeastern European countries with unused potential. Human, ecological and economic problems arising in various mountain regions have the same basic characteristics irrespective of the country. Some mountain regions are subject to specific for the conditions of the mountain and country policy for planning, development and mountain population promotion. The general goal is development of whole economy and the efficient management of natural resources and prevention of natural and tec hnological disasters. The mountain regions are one of the most threatened landscape systems in Southeastern Europe. Understanding the importance of the mountain regions and conservation of the natural heritage require scientific and institutional cooperation at all levels.

Mountains cover a quarter of the Earth's land surface and are home to about 12 percent of the global population. They are the sources of all the world's major rivers, affect regional weather patterns, provide centres of biological and cultural diversity, hold deposits of minerals, and provide both active and contemplative recreation. Yet mountains are also significantly affected by climate change; as melting and retreating glaciers show. Given the manifold goods and services which mountains provide to the world, such changes are of global importance. In this Very Short Introduction, Martin Price outlines why mountains matter at the global level, and addresses the existing and likely impacts of climate change on mountain, hydrological and ecological systems. Considering the risks associated with the increasing frequency of extreme events and 'natural hazards' caused by climate change, he discusses the implications for both mountain societies and wider populations, and concludes by emphasizing the need for greater cooperation in order to adapt to climate change in our increasingly globalized world. ABOUT THE SERIES: The Very Short Introductions series from Oxford University Press contains hundreds of titles in almost every subject area. These pocket-sized books are the perfect way to get ahead in a new subject quickly. Our expert authors combine facts, analysis, perspective, new ideas, and enthusiasm to make interesting and challenging topics highly readable.

Glaciers are considered a key and an iconic indicator of climate change. The World Glacier Monitoring Service has noted that global alpine balance has been negative for 35 consecutive years. This highlights the dire future that alpine glaciers face. The goal of this volume is to tell the story, glacier by glacier, of response to climate change from 1984-2015. Of the 165 glaciers examined in 10 different alpine regions, 162 have retreated significantly. It is evident that the changes are significant, not happening at a "glacial" pace, and are profoundly affecting alpine regions. There is a consistent result that reverberates from mountain range to mountain range, which emphasizes that although regional glacier and climate feedbacks differ, global changes are driving the response. This book considers ten different glaciated regions around the individual glaciers, and offers a different tune to the same chorus of glacier volume loss in the face of climate change.