Abstract:<p>During the last glacial period atmospheric CO<sub>2</sub> and temperature in Antarctica varied together on millennial timescales, with CO<sub>2</sub> abruptly increasing by 10-20 ppm in <1000 years in some cases. The exact causes of these rapid CO<sub>2</sub> changes during a cold glacial climate remain unclear. Here we examine the role of ocean carbon storage and atmospheric exchange by applying the bor… Show more
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