Coupled climate model simulation of El Nino/Southern Oscillation: implications for paleoclimate

G. A. Meehl; G. W. Branstator

Coupled climate model simulation of El Nino/Southern Oscillation: implications for paleoclimate

G. A. Meehl
, G. W. Branstator

Earth System Predictability

National Center for Atmospheric Research

Research output: Contribution to journal › Article › peer-review

8 Scopus citations

Abstract

A global, coarse-grid coupled ocean-atmosphere GCM is used to study climate sensitivity associated with a significant change of external forcing (a doubling of atmospheric carbon dioxide (CO₂), or 2 × CO₂). This increase of CO₂ in the model could be considered analogous to other changes in external forcing that have occurred in the paleoclimatic record. The result is a significant alteration of the amosphere-ocean circulation. -from Authors

Original language	English
Pages (from-to)	69-91
Number of pages	23
Journal	Unknown Journal
State	Published - 1993

Cite this

@article{5ec86e630049412c8bc109c73fbdc6eb,

title = "Coupled climate model simulation of El Nino/Southern Oscillation: implications for paleoclimate",

abstract = "A global, coarse-grid coupled ocean-atmosphere GCM is used to study climate sensitivity associated with a significant change of external forcing (a doubling of atmospheric carbon dioxide (CO2), or 2 × CO2). This increase of CO2 in the model could be considered analogous to other changes in external forcing that have occurred in the paleoclimatic record. The result is a significant alteration of the amosphere-ocean circulation. -from Authors",

author = "Meehl, \{G. A.\} and Branstator, \{G. W.\}",

year = "1993",

language = "English",

pages = "69--91",

journal = "Unknown Journal",

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TY - JOUR

T1 - Coupled climate model simulation of El Nino/Southern Oscillation

T2 - implications for paleoclimate

AU - Meehl, G. A.

AU - Branstator, G. W.

PY - 1993

Y1 - 1993

N2 - A global, coarse-grid coupled ocean-atmosphere GCM is used to study climate sensitivity associated with a significant change of external forcing (a doubling of atmospheric carbon dioxide (CO2), or 2 × CO2). This increase of CO2 in the model could be considered analogous to other changes in external forcing that have occurred in the paleoclimatic record. The result is a significant alteration of the amosphere-ocean circulation. -from Authors

AB - A global, coarse-grid coupled ocean-atmosphere GCM is used to study climate sensitivity associated with a significant change of external forcing (a doubling of atmospheric carbon dioxide (CO2), or 2 × CO2). This increase of CO2 in the model could be considered analogous to other changes in external forcing that have occurred in the paleoclimatic record. The result is a significant alteration of the amosphere-ocean circulation. -from Authors

UR - https://www.scopus.com/pages/publications/0027388199

M3 - Article

AN - SCOPUS:0027388199

SP - 69

EP - 91

JO - Unknown Journal

JF - Unknown Journal

ER -

Coupled climate model simulation of El Nino/Southern Oscillation: implications for paleoclimate

Abstract

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