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Relative timing of Hemispheric climate changes and atmospheric CO2 during the last deglaciation. Greenhouse 2011: The Science of Climate Change, Cairns, Australia, 4-8 April, 2011 (Ref: 14478)
Authors:
van Ommen T.Pedro J.Rasmussen S.Chappellaz J.Moy A.Morgan V.Loulergue L.Masson-Delmotte V.
Category 3: Verbal presentation

Ice Core Records of the Last Deglaciation: North-South Climate and Atmospheric CO2. Australia New Zealand Climate Forum, Hobart, September 2010, 2010 (Ref: 14251)
Authors:
Pedro J.van Ommen T.Rasmussen S.Chappellaz J.Moy A.Morgan V.Loulergue L.Masson-Delmotte V.
Category 3: Conference paper

Ice core records from Antarctic and Greenland have revealed that the last deglaciation (ca. 19, 000 to 11, 000 years before present) was accompanied by an 80 ppmv increase in atmospheric CO2 and a sequence of large, hemispheric climate variations.

A precise chronology of the last deglaciation from the Law Dome ice core International Polar Year Oslo Science Conference. Oslo, June 8-12., 2010 (Ref: 14180)
Authors:
van Ommen T.D.Pedro J.B.Chappellaz J.Loulergue L.Delmotte M.Masson-Delmotte V.Morgan V.
Category 3: Verbal presentation

During the transition from the last glacial maximum to the present warm interglacial a sequence of large, hemispheric, climate changes took place: the Bølling‐Allerød and Younger … Dryas in the north and the Antarctic Cold Reversal in the south.

The 8200 B.P. climate event in the Southern Hemisphere Geophysical Research Abstracts, 2007 (Ref: 12863)
Authors:
van Ommen T.Loulergue L.Chappellaz J.Morgan V.Spahni R.Schilt A.Curran M.MacFarling Meure C.Etheridge D.Stocker T.
Category 3: Abstract

The 8200 B.P. climate event in the Southern Hemisphere Antarctic Climate and Ecosystems CRC Symposium, Hobart, 2007, 2007 (Ref: 13162)
Authors:
van Ommen T.Loulergue L.Chappellaz J.Morgan V.Spahni R.Schilt A.Curran M.Roberts J.MacFarling Meure C.Etheridge D.Stocker T.
Category 3: Conference paper

The event that occurred approximately 8200 years ago is the largest excursion in climate since the beginning of the Holocene. In this event we observe the climatic response to a perturbation which provides a probe with which to investigate the stability of interglacial climate.

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