Paleoclimate

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A01=Michael L. Bender
Abrupt climate change
Age Group_Uncategorized
Age Group_Uncategorized
Atlantic Ocean
Author_Michael L. Bender
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Calcium carbonate
Category1=Non-Fiction
Category=RBGF
Category=RBP
Category=RBX
Cenozoic
Climate
Climate change
Climatology
COP=United States
Deep sea
Deglaciation
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Eocene
eq_isMigrated=2
eq_nobargain
Foraminifera
Global temperature
Global warming
Greenhouse effect
Greenhouse gas
Heinrich event
Holocene
Ice age
Ice core
Ice sheet
Interglacial
Intertropical Convergence Zone
Isostasy
Language_English
Little Ice Age
Medieval Warm Period
Meltwater
Methane
Methane clathrate
Monsoon
North America
Northern Hemisphere
Ocean acidification
Oligocene
PA=Available
Pacific Ocean
Paleocene
Paleocene–Eocene Thermal Maximum
Paleoclimatology
Paleogene
Paleosol
Paleozoic
Permafrost
Photorespiration
Plate tectonics
Pleistocene
Pliocene climate
Polar regions of Earth
Precambrian
Price_€20 to €50
PS=Active
Radiative forcing
Salinity
Sea
Sea ice
Sea level
Sea level rise
Sea surface temperature
Seafloor spreading
Seawater
Sediment
Snowball Earth
softlaunch
Soil
Southern Ocean
Speleothem
Stratosphere
Subtropics
Surface water
Temperate climate
Temperature record
Trade winds
Tropics
Weathering
Younger Dryas

Product details

  • ISBN 9780691145556
  • Weight: 312g
  • Dimensions: 127 x 203mm
  • Publication Date: 25 Aug 2013
  • Publisher: Princeton University Press
  • Publication City/Country: US
  • Product Form: Paperback
  • Language: English
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Earth's climate has undergone dramatic changes over the geologic timescale. At one extreme, Earth has been glaciated from the poles to the equator for periods that may have lasted millions of years. At another, temperatures were once so warm that the Canadian Arctic was heavily forested and large dinosaurs lived on Antarctica. Paleoclimatology is the study of such changes and their causes. Studying Earth's long-term climate history gives scientists vital clues about anthropogenic global warming and how climate is affected by human endeavor. In this book, Michael Bender, an internationally recognized authority on paleoclimate, provides a concise, comprehensive, and sophisticated introduction to the subject. After briefly describing the major periods in Earth history to provide geologic context, he discusses controls on climate and how the record of past climate is determined. The heart of the book then proceeds chronologically, introducing the history of climate changes over millions of years--its patterns and major transitions, and why average global temperature has varied so much. The book ends with a discussion of the Holocene (the past 10,000 years) and by putting manmade climate change in the context of paleoclimate. The most up-to-date overview on the subject, Paleoclimate provides an ideal introduction to undergraduates, nonspecialist scientists, and general readers with a scientific background.
Michael L. Bender is professor of geosciences and atmospheric/ocean sciences at Princeton University, a fellow of the American Geophysical Union, and a member of the National Academy of Sciences. He has taught paleoclimate at the graduate and undergraduate levels, and published widely on the topic in Science, Nature, and other journals.

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