The seasonal sea ice zone encompasses the region between the winter maximum and
summer minimum sea ice extent. In both the Arctic and Antarctic, the majority of the ice cover …

Recent field programs have highlighted the importance of the composite nature of the sea
ice mosaic to the climate system. Accordingly, we previously developed a process‐based …

The coupled interaction of ocean surface waves and sea ice is important in determining the
thermodynamic and dynamic properties of sea ice and its relationship to the ocean and …

Sea ice is not horizontally homogeneous on large scales. Its morphology is inherently
discrete and made of individual floes. In recent years, sea ice models have incorporated this …

Recent years have seen a rapid reduction in the summer Arctic sea ice extent. To both
understand this trend and project the future evolution of the summer Arctic sea ice, a better …

We evaluate marginal ice zone (MIZ) extent in a wave–ice 25 km-resolution coupled model,
compared with pan-Arctic wave-affected sea-ice regions derived from ICESat-2 altimetry …

The floe size distribution (FSD) is an important characteristics of sea ice, influencing several
physical processes that take place in the oceanic and atmospheric boundary layers …

The Antarctic marginal ice zone (MIZ) is a highly dynamic region where sea ice interacts with
ocean surface waves generated in ice-free areas of the Southern Ocean. Improved large …

Sea ice is a heterogeneous, evolving mosaic of individual floes, varying in spatial scales
from meters to tens of kilometers. Both the internal dynamics of the floe mosaic (floe‐floe …

Variability in sea ice conditions, combined with strong couplings to the atmosphere and the
ocean, lead to a broad range of complex sea ice dynamics. More in-situ measurements are …