The intensity of interglacial warmth in northwest Europe over the last 800,000 years: an absence of the MBE in Europe?

Candy, I.; Rose, J.; Schreve, D.; Lee, J.. 2010 The intensity of interglacial warmth in northwest Europe over the last 800,000 years: an absence of the MBE in Europe? In: AGU Fall Meeting, San Francisco, USA, 13-17 Dec 2010. (Unpublished)

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Abstract/Summary

The mid-Brunhes Event (MBE) is a climatic transition occurring between MIS 13 and 11 that separates two global climatic modes: (a) early Middle Pleistocene interglacials (780-450 ka) that are characterised by only moderate warmth and (b) Middle and Late Pleistocene interglacials (occurring after 450 ka) that are characterised by greater warmth consistent with, or warmer than, the Holocene. This event is observable within a variety of long climate records, such as SPECMAP and EPICA, but its effect on terrestrial systems is poorly understood.

Item Type:	Publication - Conference Item (Paper)
Programmes:	BGS Programmes 2010 > Geology and Landscape (England)
Additional Pages:	PP43D-06
NORA Subject Terms:	Earth Sciences
Date made live:	03 Sep 2013 10:57 +0 (UTC)
URI:	https://nora.nerc.ac.uk/id/eprint/503105

Item Type:

Publication - Conference Item (Paper)

Programmes:

BGS Programmes 2010 > Geology and Landscape (England)

Additional Pages:

PP43D-06

NORA Subject Terms:

Earth Sciences

Date made live:

03 Sep 2013 10:57 +0 (UTC)

URI:

https://nora.nerc.ac.uk/id/eprint/503105