Quantification of the spatial variability and long‐term changes of Arctic sea ice motion is
important for understanding the mechanisms of rapid Arctic sea ice decline because sea ice …

Sea-ice drift in the Antarctic marginal ice zone (MIZ) is discussed using data from a 4-month-
long drift of a buoy deployed on a pancake ice floe during the winter sea-ice expansion. We …

The annual sea ice freeze–thaw cycle plays a crucial role in the Arctic atmosphere—ice–
ocean system, regulating the seasonal energy balance of sea ice and the underlying upper …

This study presents an improved, versatile, and efficient algorithm based on the Oriented
FAST and Rotated BRIEF (ORB) combined with the maximum cross-correlation (MCC)(ORB …

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 …

Two ensembles of buoys, deployed in the marginal ice zone (MIZ) of the north-eastern
Weddell Sea region of the Southern Ocean, are analysed to characterise the dynamics …

Arctic sea ice leads are linear fractures in pack ice, which provide narrow windows for the
enhanced exchange of mass, energy, and momentum between the atmosphere and ocean …

Passive microwave remote sensing provides unique pan-Arctic light-and cloud-independent
daily coverage of lead fraction (LF) for Arctic winter and spring. In this study, we conducted a …

Sea ice is an essential component in polar regions and plays an important role in global
climate changes. Knowing sea-ice variabilities on long-term time scales is critical to …

Sea ice drift and deformation, namely sea ice dynamics, play a significant role in
atmosphere–ice–ocean coupling. Deformation patterns in sea ice can be observed over a …