375 pages, colour photos, colour illustrations, colour maps, colour tables
It's a question that has engaged climate scientists for more than a decade: Not if human activity impacts the environment, but when did that impact start to be significant? Was it in the mid-18th century, as long believed, with the Industrial Revolution producing huge amounts in greenhouse gas emissions? Or did it actually begin thousands of years earlier, as a result of the discovery and spread of agricultural practices?
Prologue Did Civilization Develop in a Naturally Warm World?
PART 1 A Mystery: Wrong-Way Greenhouse-Gas Trends
1. Natures Climatic Cycles
2. Wrong-Way Methane Trend
3. Wrong-Way Carbon Dioxide Trend
PART 2 Early Agriculture: Answer to the CO2 and CH4 Mysteries?
4. The Fertile Crescent and Europe
5. China and Southern Asia
6. The Americas
7. Africa, Australia, and Oceania
PART 3 Debating a New Hypothesis
8. Early Farming and Per Capita Land Use
9. How Should Interglacial Gas Trends Be Compared?
10. Natural Versus Anthropogenic CH4 Sources: Closer Scrutiny
11. Natural Versus Anthropogenic CO2 Sources: Closer Scrutiny
PART 4 How Science Moves Forward
13. Paradigm Shifts
14. An Emerging Paradigm for the Anthropogenic Era?
PART 5 Early Human Effects on Climate
15. Is the Next Glaciation Overdue?
16. Other Climatic Effects of Early Land Clearance
17. The End of Northern Hemisphere Glaciations
PART 6 Small Steps Back Toward an Ice Age
18. The Little Ice Age
19. Were the Drops in CO2 and CH4 Natural?
20. Mass Human Mortality and CO2 Decreases
21. Effects of Humans on Short-Term Greenhouse-Gas Reductions
There are currently no reviews for this product. Be the first to review this product!
William F. Ruddiman is retired from the University of Virginia, USA and has since concentrated his research on the climatic role farmers played during the last several thousand years by clearing land, raising livestock, and irrigating rice padis. Over the course of his career, Ruddiman has explored several different aspects of the field of paleoclimate – from orbital-scale changes in North Atlantic sediment to the cause of long-term cooling over the last 50 million years. He has written trade books and numerous journal articles.