Greenhouse Climates

M. Pagani; M. Huber; B. Sageman

doi:10.1016/B978-0-08-095975-7.01314-0

Greenhouse Climates

M. Pagani^*, M. Huber, B. Sageman

^*Corresponding author for this work

Earth and Planetary Sciences

Research output: Chapter in Book/Report/Conference proceeding › Chapter

40 Scopus citations

Abstract

This work reviews proxy records and modeling studies for the most recent greenhouse climate state and presents a broad overview of our evolving perspectives, including the primary agents forcing global climate and the feedbacks responsible for the observed temperature distributions. In this review, greenhouse climates are considered to be intervals too warm to sustain substantial continental glaciation.

Original language	English (US)
Title of host publication	The Atmosphere - History
Publisher	Elsevier Inc
Pages	281-304
Number of pages	24
Volume	6
ISBN (Print)	9780080983004
DOIs	https://doi.org/10.1016/B978-0-08-095975-7.01314-0
State	Published - Nov 2013

Keywords

Climate modeling
Glaciation
Greenhouse climate
Paleocene-Eocene thermal maximum
Temperature proxy records

ASJC Scopus subject areas

General Chemistry
General Earth and Planetary Sciences
General Environmental Science

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10.1016/B978-0-08-095975-7.01314-0

Cite this

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title = "Greenhouse Climates",

abstract = "This work reviews proxy records and modeling studies for the most recent greenhouse climate state and presents a broad overview of our evolving perspectives, including the primary agents forcing global climate and the feedbacks responsible for the observed temperature distributions. In this review, greenhouse climates are considered to be intervals too warm to sustain substantial continental glaciation.",

keywords = "Climate modeling, Glaciation, Greenhouse climate, Paleocene-Eocene thermal maximum, Temperature proxy records",

author = "M. Pagani and M. Huber and B. Sageman",

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AU - Huber, M.

AU - Sageman, B.

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AB - This work reviews proxy records and modeling studies for the most recent greenhouse climate state and presents a broad overview of our evolving perspectives, including the primary agents forcing global climate and the feedbacks responsible for the observed temperature distributions. In this review, greenhouse climates are considered to be intervals too warm to sustain substantial continental glaciation.

KW - Climate modeling

KW - Glaciation

KW - Greenhouse climate

KW - Paleocene-Eocene thermal maximum

KW - Temperature proxy records

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Greenhouse Climates

Abstract

Keywords

ASJC Scopus subject areas

Access to Document

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