Frerk Pöppelmeier studied physics at the University of Heidelberg and subsequently earned a doctorate in geosciences. As part of his dissertation, he reconstructed changes in the Atlantic circulation since the last ice age. He investigated geochemical proxies from sediment cores, especially neodymium isotopes. The ratio of the different isotopes to each other provides information about the current strength and origin of the water masses in the Atlantic. But as the young researcher has realized, “In our area of study, data alone will not get us anywhere. To get a little closer to the truth, you have to link measurement results to models”. At the OCCR, Frerk Pöppelmeier has found exactly the expertise in climate modelling that he needed to advance his research.
Harmonizing reconstructions and model simulations
Since taking up his postdoctoral position at the start of 2020, he has been working with the so-called “Bern 3D model”. Frerk Pöppelmeier emphasizes that it is “very efficiently” programmed. Because the model does not offer a particularly high resolution, it can model long periods of time quickly while incorporating additional parameters. “We are also able to take most geochemical processes into account in the simulations,” says Pöppelmeier. Equipped with the model modified according to his needs, he is now trying to find out under which conditions the tipping point of the Atlantic circulation has already been reached – or would be reached again in the future. “With the help of the model, we are investigating how the disruptive factors affect the Atlantic circulation and trying to reconcile this with the reconstructions.”