Faculty of Engineering Scholar Publishes Research in Prestigious Journal Nature
During the end of the last ice age, vast quantities of CO2, previously sequestered deep within the ocean, surged to the Southern Ocean’s surface and were released into the atmosphere, significantly contributing to global warming. However, it was theorized that some of this stored oceanic carbon might have been swept up and transported directly northward to the eastern equatorial Pacific upwelling region by Antarctic Intermediate Water (AAIW) and Subantarctic Modal Water (SAMW).