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Earth's Climate
Past and FutureThird Edition| ©2014 William F. Ruddiman
At a time when the evidence is stronger than ever that human activity is the primary cause for global climate change, William Ruddiman's breakthrough text returns in a thoroughly updated new edition. It offers a clear, engaging, objective portrait of the current state of climate science, includ...
At a time when the evidence is stronger than ever that human activity is the primary cause for global climate change, William Ruddiman's breakthrough text returns in a thoroughly updated new edition. It offers a clear, engaging, objective portrait of the current state of climate science, including compelling recent findings on anthropogenic global warming and important advances in understanding past climates.
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At a time when the evidence is stronger than ever that human activity is the primary cause for global climate change, William Ruddiman's breakthrough text returns in a thoroughly updated new edition. It offers a clear, engaging, objective portrait of the current state of climate science, including compelling recent findings on anthropogenic global warming and important advances in understanding past climates.
Features
Renowned Author
Bill Ruddiman is recognized in the science community as one of a select group of researcher/teachers with the interdisciplinary qualifications to write an authoritative textbook on EarthMultidisciplinary Presentation
The text synthesizes material from many disciplines—geology, ecology, paleobotany, glaciology, oceanography, meteorology, biogeochemistry, climate modeling, atmospheric chemistry, and hydrology, among others—into a coherent, step-by-step presentation.Focus on Major Themes
—The causes (forcing) of climate change
—The natural response times of the many components of Earth
—Interactions and feedbacks among these numerous components
—The role of carbon as it moves within the climate system at each time scale
Earth's Climate explores the climatic responses of Earth's major systems (ice, water, air, vegetation, and land) as they developed through Earth's history, moving from the earliest known climate history to historical, modern, and future changes.Mystery Solving Approach
Chapters revolve around the search for the answers as to why specific climatological phenomena occurred.Superb Art
The book is designed to showcase the art program, which features over 400 two-color illustrations (developed by the author with a grant from the National Science Foundation) depicting climatological phenomena and processes.Features Boxes
These features include discussions of climate feedbacks and interactions, tools and techniques used by climate scientists, and ongoing debates about the Earth
Bill Ruddiman is recognized in the science community as one of a select group of researcher/teachers with the interdisciplinary qualifications to write an authoritative textbook on EarthMultidisciplinary Presentation
The text synthesizes material from many disciplines—geology, ecology, paleobotany, glaciology, oceanography, meteorology, biogeochemistry, climate modeling, atmospheric chemistry, and hydrology, among others—into a coherent, step-by-step presentation.Focus on Major Themes
—The causes (forcing) of climate change
—The natural response times of the many components of Earth
—Interactions and feedbacks among these numerous components
—The role of carbon as it moves within the climate system at each time scale
Earth's Climate explores the climatic responses of Earth's major systems (ice, water, air, vegetation, and land) as they developed through Earth's history, moving from the earliest known climate history to historical, modern, and future changes.Mystery Solving Approach
Chapters revolve around the search for the answers as to why specific climatological phenomena occurred.Superb Art
The book is designed to showcase the art program, which features over 400 two-color illustrations (developed by the author with a grant from the National Science Foundation) depicting climatological phenomena and processes.Features Boxes
These features include discussions of climate feedbacks and interactions, tools and techniques used by climate scientists, and ongoing debates about the Earth
New to This Edition
New! Chapter 2. Earth's Climate System TodayThe chapter gives students a valuable foundation for understanding the basic operation of the climate system. Formerly available only online, this chapter has been integrated into the main text.Important Recent Advances
The new edition discusses a wide range of new research throughout, including the latest on:
—Cyclic orbital-scale changes in ice sheet size (Chapter 11)
—Millennial-scale changes in climate (Chapter 14)
—Responses of components of the climate system to global warming (Chapter 17)

Earth's Climate
Third Edition| ©2014
William F. Ruddiman
Digital Options

Earth's Climate
Third Edition| 2014
William F. Ruddiman
Table of Contents
Part I Framework of Climate Science
1. Overview of Climate Science
2. Earths Climate System Today
3. Climate Archives, Data, and Models
Part II Tectonic-Scale Climate Change
4. CO2 and Long-Term Climate
5. Plate Tectonics and Long-Term Climate
6. Greenhouse Climate
7. From Greenhouse to Icehouse: The Last 50 Million YearsPart III Orbital-Scale Climate Change
8. Astronomical Control of Solar Radiation
9. Insolation Control of Monsoons
10. Insolation Control of Ice Sheets
11. Orbital-Scale Changes in Carbon Dioxide and Methane
12. Orbital-Scale Interactions, Feedbacks, and Unsolved Mysteries
Part IV Glacial/Deglacial Climate Change
13. The Last Glacial Maximum
14. Climate During and Since the Last Deglaciation
15. Millennial Oscillations of ClimatePart V Historical and Future Climate Change
16. Humans and Preindustrial Climate
17. Climate Changes During the Last 1,000 Years
18. Climatic Changes Since 1850
19. Causes of Warming over the Last 125 Years
20. Future Climatic Change
Appendix 1: Isotopes of Oxygen
Appendix 2: Isotopes of Carbon
Glossary
Index
1. Overview of Climate Science
2. Earths Climate System Today
3. Climate Archives, Data, and Models
Part II Tectonic-Scale Climate Change
4. CO2 and Long-Term Climate
5. Plate Tectonics and Long-Term Climate
6. Greenhouse Climate
7. From Greenhouse to Icehouse: The Last 50 Million YearsPart III Orbital-Scale Climate Change
8. Astronomical Control of Solar Radiation
9. Insolation Control of Monsoons
10. Insolation Control of Ice Sheets
11. Orbital-Scale Changes in Carbon Dioxide and Methane
12. Orbital-Scale Interactions, Feedbacks, and Unsolved Mysteries
Part IV Glacial/Deglacial Climate Change
13. The Last Glacial Maximum
14. Climate During and Since the Last Deglaciation
15. Millennial Oscillations of ClimatePart V Historical and Future Climate Change
16. Humans and Preindustrial Climate
17. Climate Changes During the Last 1,000 Years
18. Climatic Changes Since 1850
19. Causes of Warming over the Last 125 Years
20. Future Climatic Change
Appendix 1: Isotopes of Oxygen
Appendix 2: Isotopes of Carbon
Glossary
Index
Authors

William F. Ruddiman
William F. Ruddiman was initially trained as a marine geologist. His subsequent work over many years has explored several different aspects of the field of paleoclimate. His earliest research was on orbital-scale changes in North Atlantic sediments to reconstruct past sea-surface temperatures and to quantify the deposition of ice-rafted debris. He also studied the way that vertical mixing by sea-floor organisms smoothes deep-sea climatic records. Later, his interests turned to the cause of long-term cooling over the last 50 million years. This research led to a new hypothesis that uplift of the Tibetan Plateau has been a major driver of that cooling, with Maureen Raymo's work on chemical weathering a central part of that hypothesis. That research also demonstrated that Tibetan uplift created much of the seasonally alternating monsoon climate that dominates eastern Asia today. Since entering 'semi-retirement' in 2001, Ruddiman's research has concentrated on the climatic role farmers played during the last several thousand years by clearing land, raising livestock, and irrigating rice padis. This research produced the 'early anthropogenic hypothesis' --- the idea that early agriculturalists caused an anomalous reversal in natural declines of atmospheric CO2 7000 years ago and CH4 5000 years ago. His research on this issue has been NSF-funded for several years. Because this hypothesis has been very controversial, it has provoked many studies seeking ways to test it.
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William F. Ruddiman | Third Edition | ©2013 | ISBN:9781464162312Confirm Request
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Earth's Climate
Third Edition| 2014
William F. Ruddiman
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