The effects of the Laurentide ice sheet on North American climate during the last glacial maximum

A. J. Broccoli; S. Manabe

doi:10.7202/032684ar

The effects of the Laurentide ice sheet on North American climate during the last glacial maximum

Atmospheric & Oceanic Sciences

Princeton University

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

29 Scopus citations

Abstract

A climate model, consisting of an atmospheric general circulation model coupled with a simple model of the oceanic mixed layer, is used to investigate the effects of the continental ice distribution of the last glacial maximum (LGM) on North American climate. In response to the incorporation of the expanded continental ice of the LGM, the model produces major changes in the climate of North America. -from Authors

Original language	American English
Pages (from-to)	291-299
Number of pages	9
Journal	Geographie Physique et Quaternaire
Volume	41
Issue number	2
DOIs	https://doi.org/10.7202/032684ar
State	Published - 1987

ASJC Scopus subject areas

Geology
Palaeontology

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title = "The effects of the Laurentide ice sheet on North American climate during the last glacial maximum",

abstract = "A climate model, consisting of an atmospheric general circulation model coupled with a simple model of the oceanic mixed layer, is used to investigate the effects of the continental ice distribution of the last glacial maximum (LGM) on North American climate. In response to the incorporation of the expanded continental ice of the LGM, the model produces major changes in the climate of North America. -from Authors",

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AB - A climate model, consisting of an atmospheric general circulation model coupled with a simple model of the oceanic mixed layer, is used to investigate the effects of the continental ice distribution of the last glacial maximum (LGM) on North American climate. In response to the incorporation of the expanded continental ice of the LGM, the model produces major changes in the climate of North America. -from Authors

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The effects of the Laurentide ice sheet on North American climate during the last glacial maximum

Abstract

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