Paleoclimate / / Michael L. Bender.

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 lar...

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Superior document:Title is part of eBook package: De Gruyter Princeton University Press eBook-Package Backlist 2000-2013
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Place / Publishing House:Princeton, NJ : : Princeton University Press, , [2013]
©2013
Year of Publication:2013
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Language:English
Series:Princeton Primers in Climate ; 8
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Physical Description:1 online resource (320 p.) :; 40 line illus.
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ctrlnum (DE-B1597)474392
(OCoLC)962359244
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spelling Bender, Michael L., author. aut http://id.loc.gov/vocabulary/relators/aut
Paleoclimate / Michael L. Bender.
Course Book
Princeton, NJ : Princeton University Press, [2013]
©2013
1 online resource (320 p.) : 40 line illus.
text txt rdacontent
computer c rdamedia
online resource cr rdacarrier
text file PDF rda
Princeton Primers in Climate ; 8
Frontmatter -- Contents -- Boxes -- Preface -- Acknowledgments -- 1. Earth's Climate System -- 2. The Faint Young Sun -- 3. Precambrian Glaciations -- 4. Regulation of the Earth System and Global Temperature -- 5. The Late Paleozoic Ice Ages -- 6. Equable Climates of the Mesozoic and Paleogene -- 7. The Paleocene-Eocene Thermal Maximum -- 8. The Long Cooling of the Cenozoic -- 9. The Origin of Northern Hemisphere Glaciation and the Pleistocene Ice Ages -- 10. Rapid Climate Change during the Last Glacial Period -- 11. The Holocene -- 12. Anthropogenic Global Warming in the Context of Paleoclimate -- Glossary -- Index
restricted access http://purl.org/coar/access_right/c_16ec online access with authorization star
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.
Issued also in print.
Mode of access: Internet via World Wide Web.
In English.
Description based on online resource; title from PDF title page (publisher's Web site, viewed 30. Aug 2021)
Paleoclimatology.
SCIENCE / Earth Sciences / General. bisacsh
Title is part of eBook package: De Gruyter Princeton University Press eBook-Package Backlist 2000-2013 9783110442502
print 9780691145556
https://doi.org/10.1515/9781400846375
https://www.degruyter.com/isbn/9781400846375
Cover https://www.degruyter.com/cover/covers/9781400846375.jpg
language English
format eBook
author Bender, Michael L.,
Bender, Michael L.,
spellingShingle Bender, Michael L.,
Bender, Michael L.,
Paleoclimate /
Princeton Primers in Climate ;
Frontmatter --
Contents --
Boxes --
Preface --
Acknowledgments --
1. Earth's Climate System --
2. The Faint Young Sun --
3. Precambrian Glaciations --
4. Regulation of the Earth System and Global Temperature --
5. The Late Paleozoic Ice Ages --
6. Equable Climates of the Mesozoic and Paleogene --
7. The Paleocene-Eocene Thermal Maximum --
8. The Long Cooling of the Cenozoic --
9. The Origin of Northern Hemisphere Glaciation and the Pleistocene Ice Ages --
10. Rapid Climate Change during the Last Glacial Period --
11. The Holocene --
12. Anthropogenic Global Warming in the Context of Paleoclimate --
Glossary --
Index
author_facet Bender, Michael L.,
Bender, Michael L.,
author_variant m l b ml mlb
m l b ml mlb
author_role VerfasserIn
VerfasserIn
author_sort Bender, Michael L.,
title Paleoclimate /
title_full Paleoclimate / Michael L. Bender.
title_fullStr Paleoclimate / Michael L. Bender.
title_full_unstemmed Paleoclimate / Michael L. Bender.
title_auth Paleoclimate /
title_alt Frontmatter --
Contents --
Boxes --
Preface --
Acknowledgments --
1. Earth's Climate System --
2. The Faint Young Sun --
3. Precambrian Glaciations --
4. Regulation of the Earth System and Global Temperature --
5. The Late Paleozoic Ice Ages --
6. Equable Climates of the Mesozoic and Paleogene --
7. The Paleocene-Eocene Thermal Maximum --
8. The Long Cooling of the Cenozoic --
9. The Origin of Northern Hemisphere Glaciation and the Pleistocene Ice Ages --
10. Rapid Climate Change during the Last Glacial Period --
11. The Holocene --
12. Anthropogenic Global Warming in the Context of Paleoclimate --
Glossary --
Index
title_new Paleoclimate /
title_sort paleoclimate /
series Princeton Primers in Climate ;
series2 Princeton Primers in Climate ;
publisher Princeton University Press,
publishDate 2013
physical 1 online resource (320 p.) : 40 line illus.
Issued also in print.
edition Course Book
contents Frontmatter --
Contents --
Boxes --
Preface --
Acknowledgments --
1. Earth's Climate System --
2. The Faint Young Sun --
3. Precambrian Glaciations --
4. Regulation of the Earth System and Global Temperature --
5. The Late Paleozoic Ice Ages --
6. Equable Climates of the Mesozoic and Paleogene --
7. The Paleocene-Eocene Thermal Maximum --
8. The Long Cooling of the Cenozoic --
9. The Origin of Northern Hemisphere Glaciation and the Pleistocene Ice Ages --
10. Rapid Climate Change during the Last Glacial Period --
11. The Holocene --
12. Anthropogenic Global Warming in the Context of Paleoclimate --
Glossary --
Index
isbn 9781400846375
9783110442502
9780691145556
callnumber-first Q - Science
callnumber-subject QC - Physics
callnumber-label QC884
callnumber-sort QC 3884 B39 42013EB
url https://doi.org/10.1515/9781400846375
https://www.degruyter.com/isbn/9781400846375
https://www.degruyter.com/cover/covers/9781400846375.jpg
illustrated Illustrated
dewey-hundreds 500 - Science
dewey-tens 550 - Earth sciences & geology
dewey-ones 551 - Geology, hydrology & meteorology
dewey-full 551.609/01
dewey-sort 3551.609 11
dewey-raw 551.609/01
dewey-search 551.609/01
doi_str_mv 10.1515/9781400846375
oclc_num 962359244
work_keys_str_mv AT bendermichaell paleoclimate
status_str n
ids_txt_mv (DE-B1597)474392
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carrierType_str_mv cr
hierarchy_parent_title Title is part of eBook package: De Gruyter Princeton University Press eBook-Package Backlist 2000-2013
is_hierarchy_title Paleoclimate /
container_title Title is part of eBook package: De Gruyter Princeton University Press eBook-Package Backlist 2000-2013
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