The goal of my
current research is to
better understand how the Southern Ocean CO2 sink will
evolve in the
future, when wind stress and precipitation over the Southern Ocean will
likely be higher. I am using a sector version of the MIT ocean
general
circulation and biogeochemistry model to study the impact of increasing
wind stress and precipitation on both the natural and anthropogenic CO2
fluxes from the Southern Ocean. Please refer to my poster for
some
recent results.
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