CLIMATE CHANGE RESEARCH: THE SIGNIFICANCE OF UNL’S ANDRILL PROGRAM”
January 27, 2009 Meeting
PRE REPORT: Join us on Tuesday, January 27, when our speaker will be Dr. Frank R. Rack, Executive Director of the ANDRILL Science Management Office at UNL. The ANDRILL Program is a multinational effort to understand climate records from sites proximal to Antarctica’s ice margins by investigating long sediment cores recovered from the continental margin. ANDRILL’s science objectives are to explore Antarctica’s response to climatic forcing over a wide range of boundary conditions, to address how changes in the Antarctic environment are represented in the geologic archive provided by sedimentary rock cores, and to understand how these records inform us about changes that might be expressed in the future. The Antarctic cryosphere (ice sheets, ice shelves, sea-ice) and marginal seas play fundamental roles in the global ice/ocean/climate system. Obtaining a history of Antarctica’s response to local, regional, and global forcing is critical for understanding past and future ice-ocean-atmospheric circulation and feedbacks within Earth’s climate system. Join us on Tuesday for a brief overview of the ANDRILL Program and a discussion of its significance in the broad scope of the science of climate change.
POST REPORT: It’s simply amazing what you can learn by studying dirt...well, the more proper term would be sediment cores. For example, by studying cores from thousands of feet below the earth’s surface, we’ve learned that there’s a proven correlation between CO2 (carbon dioxide) levels and the average temperature of the atmosphere. Dr. Frank Rack, Executive Director of the University of Nebraska ANDRILL Program (http://www.andrill.org/), focused on obtaining and analyzing sediment cores from the core of the earth near the South Pole, noted that the studies so far have clearly shown that the earth has gone through some 50 cycles of warming then cooling. In each instance, a rise in CO2 was accompanied by a rise in temperature. The information about these cycles comes from the sediment core samples that date back some six million years. The ANDRILL Program involves some 45 scientists who oversee a program to drill into the earth’s core from an ice shelf in the Antarctic. Each summer they drill for 90 to 120 days when they can set up the equipment and go deep enough to access sediment for analysis. Funding for the program comes from the National Science Foundation. The resulting data contributes to worldwide studies focused on long-term changes that we can predict into the future by looking at changes in the past.








