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A growing body of scientific evidence suggests that greenhouse-gas pollution is largely responsible for global warming. Yet, it is also true that the climate system varies quite naturally on different time-scales. Accurately predicting the course of future climate change requires an understanding of the natural variability of the climate system, as well as the effects of human-induced change. This ground-breaking book addresses predictable modification in the climate system in the context of global warming. Ideal for researchers and advanced students, it explores current thinking on natural…mehr

Produktbeschreibung
A growing body of scientific evidence suggests that greenhouse-gas pollution is largely responsible for global warming. Yet, it is also true that the climate system varies quite naturally on different time-scales. Accurately predicting the course of future climate change requires an understanding of the natural variability of the climate system, as well as the effects of human-induced change. This ground-breaking book addresses predictable modification in the climate system in the context of global warming. Ideal for researchers and advanced students, it explores current thinking on natural climate change, the use of models to simulate past climate variability, and the role of past climate variability in explaining current changes to ecosystems and society over the later part of the Holocene. The volume provides the groundwork for making critical decisions about the earth's future, and contributes substantially to the ongoing debate over global warming and climate change.
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Autorenporträt
Rick Battarbee is Professor of Environmental Change and Director of the Environmental Change Research Centre at UCL. He is a Fellow of the Royal Society and a Foreign Member of the Norwegian Academy of Science and Letters and was the Chair of the European Science Foundation program "HOLIVAR." Heather Binney is a Research Fellow in the Environmental Change Research Centre, UCL. She is a palynologist with a special interest in pollen-vegetation relationships.
Rezensionen
"Volumessuch as this provide the historical contexts and broad overviewsneeded to advance climate change biology toward broader conceptualdevelopments and synthetic methodologies for understanding andpredicting climate change effects, as well as developing effectiveadaptation and mitigation strategies.". (The Quarterly Review ofBiology, 1 December 2010)

"Thisis an important book for understanding climate changes in a longerperspective." (Geologos,2010)

"This bookbrings together some of the most prolific names in their field tocreate a sound and interesting look into this area." (TheEnvironmentalist, November2009)

"It highlights the need to improve not only ourunderstanding of the physical system through time but also ourknowledge of human influence on the climate system and viceversa." (Bulletin of the American Meteorological Society, April 2009)

"Although aimed at 'researchers and advancedstudents', this layman found the book perfectlyaccessible." (Geoscientist, August 2009)

"The rapid climate change that seems to be occurring world-widemake this volume both timely and instructive, concentrating as itdoes on the Holocene period.... An essential addition for anmeteorological library." (The International Journal ofMeteorology, April 2009)

The Holocene, the interval covered by the last 12,000 years,represents a largely nonglacial period in Earth's climaticevolution. This book synthesizes the climate history of thisinterval and investigates the role of natural climate variabilityin explaining current global warming. The volume contains tenchapters written by experts in various aspects of past climatechange. Chapter 1 provides a short introduction and outlines theobjectives/contents of subsequent chapters. The next chapter, thelongest (51 pages), considers the progress, paradigms, and problemsin Holocene climate research. Chapter 3 addresses the fundamentalquestion of the human role in the changing climate of the Holocenewhile acknowledging that climate change itself has stronglyimpacted the history of civilizations. Our ability to predictfuture climate depends on our ability to reconstruct and model whathas already happened; chapter 4 explores this vital issue.Subsequent chapters examine some relevant intervals including theso-called Holocene thermal optimum, and evaluate and model whatnatural processes might have contributed to observed climatehistories. The final chapters assess rapid land-cover change andanalyze future climate change within the perspective of the last12,000 years. Includes chapter references, an eight-page index, anda three-page summary of abbreviations and dating conventions.Summing Up: Recommended. Graduate students, researchers,faculty, professional audiences. -- J. T. Andrews, University ofColorado at Boulder (Choice, February 2009)…mehr