These areas are located in the westerly wind zone of the southern hemisphere — a look into their past climates is central for Li's research. And: There are peat bogs there, a particularly interesting climate archive if you are interested in mercury isotopes. That's because these enter the soil mainly via rain, and in turn, the amount of rain is directly related to wind strength. In other words, mercury isotopes are a so-called proxy for rain and thus for wind. "I will deliver the first quantitative reconstruction of how the dynamics of westerly winds in the Southern Hemisphere have changed over the past 17,000 years," Li promises. This information could help explain under which conditions the Southern Ocean functions as a CO2 sink and when it functions as a source of CO2. After all, the strength of the wind is the decisive factor for ocean circulation and the carbon cycle.
What's unique about Li's approach is that she wants to prove the link between rainfall and wind strength using measured data — the concentration of mercury isotopes in peat cores. "So far, these are theoretical considerations," she explains, "it won't be easy to prove them empirically." Hasn't anyone done that yet? "No, that's just the thing!" bursts out Chuxian Li. "This is a brand new idea, which is why I'm fighting so hard for this project," she beams.
(January 2023)