Danny Sigman and Ellen Ai solve glacial cycle mystery (IMAGE)
Caption
Since the discovery that atmospheric carbon dioxide (CO2) concentrations were lower during past ice ages, the cause has been a mystery. Now, Princeton geoscientists Danny Sigman and Ellen Ai (seen here in 2019, at left with other graduate student members of the Sigman Lab) have discovered that a weakening in upwelling in the Antarctic Ocean, the ocean around Antarctica, kept more CO2 in the deep ocean during the ice ages. This brings scientists closer to a complete explanation for the climate cycle between the ice ages and warm periods such as today. This also suggests that upwelling will strengthen under human-driven global warming, altering the concentration of atmospheric CO2, global climate and ocean ecosystems.
Credit
Laura Pedrick
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