Study links Northern Hemisphere ice sheets to Southern Ocean carbon storage
Research from the University of St Andrews, published in the Journal of Climate, proposes a mechanism by which growing Northern Hemisphere ice sheets cool North Atlantic waters that travel through global circulation to alter conditions around Antarctica and boost deep-ocean CO2 storage. In simulations, cooling only the northernmost latitudes produced 74% of the atmospheric CO2 reduction seen when the entire planet was cooled.
- Cooling only northern waters produced 74% of the CO2 drop from full-planet cooling
- Mechanism connects Northern Hemisphere ice growth to Antarctic ocean circulation
- Result comes from an idealized model, not a specific past ice age
- The study appeared in the Journal of Climate on October 22, 2026
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