Climate Changes During The Holocene And Their Impact On Hydrological Systems

This volume provides a comprehensive review of the effects of climate variability on hydrological and human systems in the Holocene (last 10, 000 years), with a view to predicting similar effects in the future. It will be of value to researchers and professionals in hydrology, climatology, geology and historical geography.

It is now widely accepted that increasing concentrations of greenhouse gases in the atmosphere are causing higher global temperatures. This volume provides a comprehensive review of the effects of climate variability on hydrological and human systems in the Holocene (the last 10,000 years). The book concentrates on the regions bordering the Mediterranean Sea, western and central Europe, China, Japan, West and South Africa and southwestern U.S.A. It is intended for researchers and professionals in hydrology, climatology, geology and historical geography.

It is now widely accepted that increasing concentrations of greenhouse gases in the atmosphere are causing higher global atmospheric temperatures. However, there is still a great deal of uncertainty about the likely effects of such a temperature rise on climate, and even more about the impacts of climate change and variability on the world's hydrological regimes and socio-economic systems. Studying the effects of climate variability in the past can give clues as to possible future effects. This volume provides a comprehensive review of the effects of climate variability on hydrological and human systems in the Holocene (the last 10,000 years), in various parts of the world. The book concentrates on the regions bordering the Mediterranean Sea, western and central Europe, China, Japan, West and South Africa and the southwestern USA. This book will be of value to researchers and professionals in hydrology, climatology, geology and historical geography.

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.

Holocene Climate Change and Environment presents detailed, diverse case studies from a range of environmental and geological regions on the Indian subcontinent which occupies the central part of the monsoon domain. This book examines Holocene events at different time intervals based on a new, high-resolution, multi-proxy records (pollen, spores, NPP, diatoms, grain size characteristics, total organic carbon, carbon/nitrogen ratio, stable isotopes) and other physical tools from all regions of India. It also covers new facilities in chronological study and luminescence dating, which have added a new dimension toward understanding the Holocene glacial retreats evolution of coastal landforms, landscape dynamics and human evolution. Each chapter is presented with a unified structure for ease of access and application, including an introduction, geographic details, field work and sampling techniques, methods, results and discussion. This detailed examination of such an important region provides key insights in climate modeling and global prediction systems. Provides data and research from environmentally and geologically diverse regions across the Indian subcontinent Presents an integrated and interdisciplinary approach, including considerations of human impacts Features detailed case studies that include methods and data, allowing for applications related to research and global modeling

Since the greenhouse effect emerged as a predictable threat, necessitating the evalu ation of its future impact on the environment in the various parts of the globe, interest in the climate changes during the Holocene has gained momentum. The background can be summarized by the sentence: The past is a key to the future. As a matter of fact, this sentence is in the opposite direction, on the dimension of time, to the principle adopted by the founders of the science of geology. They proposed that geological processes in the present should be used as a key for understanding the past. Another reason for the interest in the history of the climate of the Holocene can be described as the renaissance of a modified deterministic approach to the inter relation between physical and human geography. This relates in the first place to the fact that various investigations, especially as carried out by Hubert Lamb, showed that the sequence of climate changes previously suggested by Blytt and Sernander for Europe and adopted by most Holocene climatologists was far too general, and that there were more climate changes during recent history than previously taken account of. In the second place it was found out that these changes had had an impact on the history of human communities. Thus, one can conclude that once the taboo on geographical determinism (i. e.

An in-depth overview of the role of the hydrological cycle within the climate system, including climate change impacts on hydrological reserves and fluxes, and the controls of terrestrial hydrology on regional and global climatology. Table of contents : 1. The Role of the Hydrological Cycle in the Climate System 2. Evaporation 3. Physics of Evaporation and Atmospheric Boundary Layers Over Land 4. Precipitation Physics and Rainfall Observation 5. Land Surface Hydrology 6. Land Surface Schemes and Climate Models 7. Arctic and Snow Hydrology 8. Dynamics of Glaciers, Ice Sheets and Global Sea Level 9. Feedback Mechanisms : Precipitation and Soil Moisture 10. Feedback Mechanisms : Land Use, Hydrology and Carbon 11. Palaeohydrology : An Introduction 12. Groundwater Palaeohydrology 13. Global Warming and the Acceleration of the Hydrological Cycle 14. Climate Change and Hydrological Impact Studies 15. Remote Sensing for Hydrological Studies

Experts in climate and water sciences from Canada, the United States, Brazil, Denmark, Germany, Belgium, France, Serbia, and other European countries and the UNESCO gathered at the Serbian Academy of Sciences and Arts on the occasion of the 130th birthday anniversary of the geophysicist Milutin Milankovitch. The collection of their presentations is opened by an update on the climate situation after the Fourth Assessment Report of the Intergovernmental Panel on Climate Change. Further topics include various issues of paleoclimatology, in particular as it helps reduce uncertainties from which prospects for climate change suffer; ecohydrology and climate change at the watershed scale; and regional climate models, which are discussed in terms of both their improved modeling and their use in studies of a polynya in the Antarctica and expected changes in the Mediterranean region.