Antarctic Ice - Cold Shoulder to Warming Trends
- Atmospheric Circulation: Changes in atmospheric circulation have led to more sea ice being carried to the coast by wind, stabilizing ice shelves.
- Ocean Surface Cooling: Antarctic sea ice has expanded due to ocean surface cooling associated with multidecadal variability in the Southern Ocean.
- Complex InteractionsThe Antarctic sea ice is influenced by a variety of factors, including sub-ice-shelf melting, stratospheric ozone depletion, and tropical teleconnections.
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Expect ice-free Arctic summer within 15 years
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