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This transcript may not be quoted, reproduced or redistributed in whole or in part by any means except with the written permission of the American Institute of Physics. This transcript is based on a tape-recorded interview deposited at the Center for History of Physics of the American Institute of Physics. The AIP's interviews have generally been transcribed from tape, edited by the interviewer for clarity, and then further edited by the interviewee. If this interview is important to you, you should consult earlier versions of the transcript or listen to the original tape. For many interviews, the AIP retains substantial files with further information about the interviewee and the interview itself.
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Travelling in Time through Climate History

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Coral carbon isotope sensitivity to growth rate and water depth with paleo-sea level implications

When climatologists look into the past, they intend to learn for the future. Victor Brovkin and his team at Hamburg's Max Planck Institute for Meteorology reconstruct historical climate changes and analyze what processes reinforce those changes. Their discoveries are helping to predict the future of the Blue Planet. Victor Brovkin comes across as a reserved and patient interviewee, but on one subject he expresses himself in blunt and adamant terms:
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Jump to navigation. We know a lot about how carbon dioxide CO 2 levels can drive climate change, but how about the way that climate change can cause fluctuations in CO 2 levels? New research from an international team of scientists reveals one of the mechanisms by which a colder climate was accompanied by depleted atmospheric CO 2 during past ice ages. Pomona College Visiting Scholar in Geology Maria Prokopenko was among the scientists investigating how and why the earth goes through periodic climate change, which could shed light on how man-made factors could affect the global climate. Earth's average temperature has naturally fluctuated by about 4 to 5 degrees Celsius over the course of the past million years as the planet has cycled in and out of glacial periods.

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