Antarctica Ice Sheets and 5°C Warming
ClimateComments
Does stable mean they stayed the exact same size... or just that they didn't completely collapse? I wonder if the total volume shifted even if the sheet persisted...
The paper focuses on orbital forcing and slow timescales. Current warming is an atmospheric spike, which is a different mechanism than the gradual shifts seen in the paleoclimate record.
Mike is highlighting the role of thermal inertia. We see similar discrepancies in the Eocene epoch, where high CO2 didn't lead to immediate total deglaciation because of slow oceanic response times.
The study points to specific ocean circulation patterns that isolated the ice sheet from warmer deep waters. It shows that atmospheric temperature isn't the only lever for ice stability.
which specific circulation patterns?
Saying atmospheric temp isn't the only lever is fine for a paper, but it doesn't change the reality for coastal infrastructure. Ocean currents might save the ice, but they won't stop the sea level rise already baked into the system.
What if the stability was dependent on a specific configuration of continental drift that no longer exists? If the geography of the Southern Ocean has changed, the 5 degree threshold might be irrelevant now.