In an article published by Eos, Jean Lynch-Stieglitz, chair of the School of Earth and Atmospheric Sciences, comments on a new study published in Nature which found that a major part of the Atlantic Meridional Overturning Circulation (AMOC) was warmer during the peak of Earth’s last ice age than previously thought.

According to Lynch-Stieglitz, the findings give scientists an additional benchmark with which to test the accuracy of climate models. “Last Glacial Maximum (LGM) circulation is a good target, and the more that we can refine the benchmarks…that’s a really good thing,” she said. “This is another really nice dataset that can be used to better assess what the Last Glacial Maximum circulation was really doing.”