The ice-ocean interface is a dynamic zone characterized by the transfer of heat, salinity, and
energy. Complex thermodynamics and fluid dynamics drive fascinating physics as ice is …

A summary is given on the utility of laboratory experiments for gaining understanding of
wave attenuation in the marginal ice zone, as a complement to field observations, theory …

Irregular, unidirectional surface water waves incident on model ice in an ice tank are used
as a physical model of ocean surface wave interactions with sea ice. Results are given for …

In the marginal ice zone (MIZ), where ocean waves and sea ice interact, waves can produce
flows of water across ice floe surfaces in a process known as wave overwash. Overwash …

Sea ice attenuates waves propagating from the open ocean. Here, we model the evolution
of energetic unidirectional random waves in the marginal ice zone with a nonlinear …

The marginal ice zone is a highly dynamical region where sea ice and ocean waves interact.
Large-scale sea ice models only compute domain-averaged responses. As the majority of …

Wave–ice interactions were investigated experimentally to understand the waves
transmitted by the freely floating model ice floes and mean drift velocity of them in a three …

The evolution of ice conditions and wave patterns in polar water areas is complex, and
studying the hydrodynamic response between sea ice and waves is crucial. In this study, the …

Over recent decades, the Arctic Ocean has experienced dramatic variations due to climate
change. By retreating at a rate of 13% per decade, sea ice has opened up significant areas …

Estimates of directional wave spectra and related parameters can be obtained from ship
motion data through the wave-buoy analogy approach. The fundamental input is the …