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New constraints on north-south climate coupling and the CO2/temperature relation during the last deglaciation from polar ice cores. First Australian Earth System Outlook Conference, Australian Academy of Science, Canberra. December 9-10., 2010 (Ref: 14276)
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 a ca. 80 ppmv increase in atmospheric CO2 and a sequence of large, hemispheric climate variations.

Ice Core Records of the Last Deglaciation: North-South Climate and Atmospheric CO2. Australia New Zealand Climate Forum, Hobart, September 2010, 2010 (Ref: 14251)
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)
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.

Firn-air del15N in modern polar sites and glacial-interglacial ice: a model-data mismatch during glacial periods in Antarctica? Quaternary Science Reviews, 2006 (Ref: 12243)
Category 1: Peer-reviewed literature

The phase lag between atmospheric composition (air bubbles) and temperature (water isotopes) can be quantified from ice cores provided that the age difference between entrapped air and the surrounding air can be correctly estimated. This difference depends on the lock-in depth (LID)…

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