MARUM Research Academy
2025
© U. Röhl, MARUM and IODP
The Topic
The Southern Ocean and Antarctic ice sheet stability play a critical role for global ocean circulation, climate, the marine carbon cycle and global sea level. A major feature is the Antarctic Circumpolar Current (ACC) as the world’s largest ocean current system controlled by atmospheric forcing, oceanic density gradients, and eddy activity. The ACC connects all three major basins of the global ocean and therefore integrates, and responds to, climate signals throughout the globe. While reconstructions of southern, high-latitude paleoclimate are still sparse, recent years have seen much progress, including a multitude of land and sea-based coring efforts, key IODP expeditions and work on legacy sediment cores. These studies suggest for example regional heterogeneity in ACC position and strength over the Pleistocene glacial-interglacial cycles, while the long-term evolution of the ACC is still comparatively poorly known. Recent IODP expeditions in the subantarctic South Pacific allowed to reconstruct ACC changes over the past five million years, showing strong ~400,000-year eccentricity cycles, likely originating from modulation of precessional changes linked to tropical Pacific temperature variability.
Sponsors
|
Contact: |
|