Permafrost Hydrology

Permafrost Hydrology systematically elucidates the roles of seasonally and perennially frozen ground on the distribution, storage and flow of water. Cold regions of the World are subject to mounting development which significantly affects the physical environment. Climate change, natural or human-induced, reinforces the impacts. Knowledge of surface and ground water processes operating in permafrost terrain is fundamental to planning, management and conservation. This book is an indispensable reference for libraries and researchers, an information source for practitioners, and a valuable text for training the next generations of cold region scientists and engineers.

This book provides a comprehensive, up-to-date assessment of the key terrestrial components of the Arctic system, i.e., its hydrology, permafrost, and ecology, drawing on the latest research results from across the circumpolar regions. The Arctic is an integrated system, the elements of which are closely linked by the atmosphere, ocean, and land. Using an integrated system approach, the book’s 30 chapters, written by a diverse team of leading scholars, carefully examine Arctic climate variability/change, large river hydrology, lakes and wetlands, snow cover and ice processes, permafrost characteristics, vegetation/landscape changes, and the future trajectory of Arctic system evolution. The discussions cover the fundamental features of and processes in the Arctic system, with a special focus on critical knowledge gaps, i.e., the interactions and feedbacks between water, permafrost, and ecosystem, such as snow pack and permafrost changes and their impacts on basin hydrology and ecology, river flow, geochemistry, and energy fluxes to the Arctic Ocean, and the structure and function of the Arctic ecosystem in response to past/future changes in climate, hydrology, and permafrost conditions. Given its scope, the book offers a valuable resource for researchers, graduate students, environmentalists, managers, and administrators who are concerned with the northern environment and resources.

1. Predicting the Hydrological Effects of Climate Change.- Section I Sensitivity of the Global Hydrosphere Section Summary.- 2. An Introduction to Global Water Dynamics.- 3. Modelling the Biospheric Aspects of the Hydrological Cycle: Upscaling Processes and Downscaling Weather Data.- 4. Trends in Historical Steamflow Records.- Section II Regional Implications of Global Warming Section Summary.- 5. Hydrology of Northern North America under Global Warming.- 6. Current Evidence on the Likely Impact of Global Warming on Hydrological Regimes in Europe.- 7. The Impact of Climatic Warming on Hydrological Regimes in China: An Overview.- Section III Precipitation Change and Variability Section Summary.- 8. The Influence of Topography, Season and Circulation on Spatial Patterns of Daily Precipitation.- 9. Use of Artificial Neural Networks in Precipitation Forecasting.- 10. Generation of Sequences of Air Temperature and Precipitation for Estimation of the Hydrological Cycle in Changing Climatic Conditions in Poland.- 11. Some Aspects of Climatic Fluctuation at Four Stations on the Tibetan Plateau during the Last 40 Years.- 12. The Influences of the North Atlantic Oscillation, the El Niño/Southern Oscillation and the Quasi-Biennial Oscillation on Winter Precipitation in Ireland.- Section IV Impacts on Snow, Ice and Meltwaters Section Summary.- 13. Runoff Formation and Discharge Modelling of a Glacierized Basin in the Tianshan Mountains.- 14. Impact of Future Climate Change on Glacier Runoff and the Possibilities for Artificially Increasing Melt Water Runoff in the Aral Sea Basin.- 15. Glaciers and Snowcover in Central Asia as Indicators of Climate Change in the Earth-Ocean-Atmosphere System.- 16. Global Warming and the Trend toward Dryness in the Frigid High Mountains and Plateau of Western China.- Section V The Water Balance and Changing Regional Resources Section Summary.- 17. A Method to Assess the Effects of Climatic Warming on the Water Balance of Mountainous Regions.- 18. Sensitivity Analyses for the Impact of Global Warming on Water Resources in Wales.- 19. Potential Hydrological Responses to Climate Change in Australia.- 20. Dynamics of Stage Fluctuation in Yangzhouyongcuo Lake, Tibetan Plateau.- 21. Derivation of Surface Temperature, Albedo, and Radiative Fluxes over the Tibetan Plateau Based on Satellite Measurement.- 22. Climatic Warming and its Impact on the Water Resources of the Yalong River, China.- 23. The Probable Impact of Global Change on the Water Resources of Patagonia, Argentina.- 24. Long Term Trends in the Water Balance of Central Japan.- Conclusions.- 25. The Impact of Global Warming on Regional Hydrology and Future Research Priorities.

This survey of current knowledge and research in hydrology in the Canadian north includes data on climate snow, permafrost, ground water, floating ice, glaciers, water quality and the regional energy balance.

The introduction of the term periglacial by Lozinski in 1909 to describe the cold-climate conditions in the zone adjacent to, but beyond, the Pleistocene glaciers encouraged the separate development of geocryological and glaciological research. Geological and geomorphological processes at the interface between glaciers and permafrost have, as a result, been given less attention than they warrant, and the influence of one on the other has in many respects been neglected. This book includes a collection of papers that emphasize glacier-permafrost interactions. Papers consider permafrost and its influence on glacitectonic processes, glacial meltwater systems and ground-ice development in proglacial and ice-marginal environments. In addition, recent research findings are reported on paraglacial processes, permafrost evolution, rock glaciers, the formation of ice-wedge casts and periglacial slope evolution. It is hoped that this book will stimulate interest in the interface between glacial and periglacial systems, and encourage further collaborative research involving glaciologists and glacial geologists on the one hand, and geocryologists and permafrost scientists on the other.