The long thaw : how humans are changing the next 100,000 years of Earth's climate /

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Bibliographic Details
Author / Creator:Archer, David, 1960-
Imprint:Princeton, N.J. ; Oxford : Princeton University Press, c2009.
Description:ix, 180 p. : ill., maps ; 22 cm.
Language:English
Series:Science essentials
Science essentials (National Academy of Sciences (U.S.))
Subject:
Format: Print Book
URL for this record:http://pi.lib.uchicago.edu/1001/cat/bib/7469117
Hidden Bibliographic Details
ISBN:9780691136547 (hbk.)
0691136548 (hbk.)
Notes:Includes bibliographical references and index.
Table of Contents:
  • Acknowledgments xi
  • Prologue
  • Global Warming in Geologic Time
  • An overview of the thrust of the book: human-induced climate change in the context of geologic time, in the past and in the future
  • Section I. The Present
  • Chapter 1. The Greenhouse Effect
  • Fourier and greenhouse theory Early CO 2 measurements Arrhenius and the forecast
  • Climate science since then
  • Chapter 2. We've Seen It with Our Own Eyes
  • Testing the forecast Impacts already
  • Chapter 3. Forecast of the Century
  • A century-timescale climate spike Temperature, rainfall, sea level, and storms
  • Section II. The Past
  • Chapter 4. Millennial Climate Cycles
  • Abrupt climate transitions, and climate cycles on millennial timescales
  • The Little Ice Age and the Medieval Optimum climates
  • Chapter 5. Glacial Climate Cycles
  • History of their discovery Ice flows and melts in quirky ways
  • Orbital forcing and CO 2 forcing
  • Chapter 6. Geologic Climate Cycles
  • Our ice age is unusual
  • The Earth is breathing
  • Chapter 7. The Present in the Bosom of the Past
  • Climate change so far and in the coming century, compared with deglaciation, abrupt climate change, the Eocene hothouse, the Paleocene/Eocene thermal maximum event, and the K/T boundary
  • Section III. The future
  • Chapter 8. The Fate of Fossil Fuel CO 2 Reservoirs of carbon, breathing
  • New carbon from fossil fuels equilibrates with the ocean and the land
  • Chapter 9. Acidifying the Ocean
  • CO 2 is an acid CaCO 3 is a base
  • Neutralization takes millennia
  • CO 2 remains higher than natural for hundreds of millennia
  • Chapter 10. Carbon Cycle Feedbacks
  • The short-term prognosis
  • The long-term prognosis
  • Chapter 11. Sea Level in the Deep Future
  • If the past is the key to the future, we have the capacity to raise sea level by 50 meters, eventually
  • Chapter 12. Orbits, CO 2 , and the Next Ice Age
  • Interplay between orbital and CO 2 climate forcings
  • The next ice age is about to be canceled
  • Epilogue: Carbon Economics and Ethics
  • What the options are and how we decide
  • Further Reading
  • Index