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Carrie Lear, Cardiff Universityย
Since 1992, loss of ice from the Antarctic ice sheet has contributed 8 mm to global sea level rise, with 40% of this occurring in the last 5 years. The future loss of ice from Antarctica represents the largest uncertainty in future global sea level predictions. This is concerning because the Antarctic ice sheet is large enough to raise global sea level approximately 65 m if it were to melt completely.
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As Earth Scientists, we know that Earthโs climate has changed naturally in the past. Can we use the past behaviour of the Antarctic ice sheet to predict its future behaviour in a warming climate? To do this we would need to reconstruct a record of ice sheet volume through time. However, this is not straightforward because the ice sheet itself has obliterated or covered most of the direct evidence for its past advance and retreat on Antarctica. In this lecture I first of all explain how we use indirect methods to reconstruct changes in the size of the Antarctic ice sheet millions of years in the past. We will see how the formation of the ice sheet approximately 34 million years ago made its mark in marine geochemical proxy records. I will then show that these records reveal a surprisingly dynamic history of the Antarctic ice sheet, with worrying implications for future ice sheet stability.
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17.30 Registration
18.00 Lecture begins
18.45 Questions and answers
19.00 Lecture ends and there is a short soft drinks reception in the lower library
20.00 Close
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For more information, please check out the websiteย www.geolsoc.og.uk