A multi-model assessment of last interglacial temperatures
The last interglaciation (~130 to 116 ka) is a time period with a strong astronomically induced seasonal forcing of insolation compared to the present. Proxy records indicate a significantly different climate to that of the modern, in particular Arctic summer warming and higher eustatic sea level. B...
Main Authors: | , , , , , , , , , , , , , , , , , , , , , , , , , , , |
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Format: | Article |
Language: | English |
Published: |
Copernicus Publications
2013-03-01
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Series: | Climate of the Past |
Online Access: | http://www.clim-past.net/9/699/2013/cp-9-699-2013.pdf |