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| 010 | _z 2013011814 | ||
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| 080 | _a551.583 | ||
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_a551.609/01 _223 |
| 049 | _aMAIN | ||
| 100 | 1 |
_aBender, Michael L., _eauthor. _964724 |
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| 245 | 1 | 0 |
_aPaleoclimate / _cMichael L. Bender. |
| 264 | 1 |
_aPrinceton, New Jersey : _bPrinceton University Press, _c[2013] |
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| 300 |
_a1 online resource (xi, 306 pages) : _billustrations |
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| 336 |
_atext _btxt _2rdacontent |
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| 337 |
_acomputer _bc _2rdamedia |
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_aonline resource _bcr _2rdacarrier |
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| 490 | 1 | _aPrinceton primers in climate | |
| 504 | _aIncludes bibliographical references and index. | ||
| 505 | 0 | _aEarth's climate system -- The faint young sun -- Precambrian glaciations -- Regulation of the Earth system and global temperature -- The late Paleozoic ages -- Equable climates of the Mesozoic and Paleogene -- The Paleocene-Eocene thermal maximum -- The long cooling of the Cenozoic -- The origin of Northern Hemisphere glaciation and the Pleistocene ice ages -- Rapid climate change during the last glacial period -- The Holocene -- Anthropogenic global warming in the context of paleoclimate. | |
| 588 | 0 | _aPrint version record. | |
| 520 | _a'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."--Provided by publisher. | ||
| 546 | _aEnglish. | ||
| 590 |
_aIEEE _bIEEE Xplore Princeton University Press eBooks Library |
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| 650 | 0 |
_aPaleoclimatology. _964164 |
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| 650 | 6 |
_aPal�eoclimatologie. _964169 |
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| 650 | 7 |
_aSCIENCE _xEarth Sciences _xGeography. _2bisacsh _96043 |
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| 650 | 7 |
_aSCIENCE _xEarth Sciences _xGeology. _2bisacsh _96044 |
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| 650 | 7 |
_aSCIENCE _xEarth Sciences _xMeteorology & Climatology. _2bisacsh _964725 |
|
| 650 | 7 |
_aPaleoclimatology. _2fast _0(OCoLC)fst01051364 _964164 |
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| 650 | 7 |
_aPal�aoklima _2gnd _964726 |
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| 655 | 4 |
_aElectronic books. _93294 |
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| 776 | 0 | 8 |
_iPrint version: _aBender, Michael L. _tPaleoclimate. _dPrinceton, New Jersey : Princeton University Press, 2013 _z9781400846375 _w(DLC) 2013011814 _w(OCoLC)820123451 |
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_aPrinceton primers in climate. _963881 |
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