Observed Arctic sea ice losses are a sentinel of anthropogenic climate change. These
reductions are projected to continue with ongoing warming, ultimately leading to an ice-free …

Arctic sea ice mediates atmosphere-ocean momentum transfer, which drives upper ocean
circulation. How Arctic Ocean surface stress and velocity respond to sea ice decline and …

The Arctic has been suggested to see seasonally ice-free conditions within two-to-three
decades under high-emissions scenarios. However, the time of emergence of the first ice …

The Arctic sea-ice cover is strongly influenced by internal variability on decadal timescales,
affecting both short-term trends and the timing of the first ice-free summer. Several …

New Potential to Reduce Uncertainty in Regional Climate Projections by Combining Physical
and Socio‐Economic Constraints - Lehner - 2023 - AGU Advances - Wiley Online Library Skip …

Although the trend of sea-ice extent under global warming has been studied extensively in
recent years, most climate models have failed to capture the recent rapid change in the …

Future projections of Arctic and Antarctic sea ice suffer from uncertainties largely associated
with inter-model spread. Ocean heat transport has been hypothesised as a source of this …

Arctic sea ice has steadily diminished as atmospheric greenhouse gas concentrations have
increased. Using observed data from 1979 to 2019, we estimate a close contemporaneous …

Sea ice (including overlying snow) is a dynamic interface between the atmosphere and the
ocean, influencing the mercury (Hg) cycling in polar oceans. However, a large-scale and …