The propagation of ocean surface waves within the marginal ice zone (MIZ) is a defining
phenomenon of this dynamic zone. Over decades of study, a variety of methods have been …

There has been a significant increase of studies on wave–ice interactions in the past
decades. Through a close look at a representative set of theories, this paper investigates …

Wave and sea ice properties in the Arctic and Southern Oceans are linked by feedback
mechanisms, therefore the understanding of wave propagation in these regions is essential …

The marginal ice zone (MIZ) is the dynamic interface between the open ocean and sea ice-
covered ocean. It is characterized by interactions between surface gravity waves and …

The attenuation of ocean surface waves during seasonal ice cover is an important control on
the evolution of Arctic coastlines. The spatial and temporal variations in this process have …

ABSTRACT A drifting wave-ice buoy (Medusa-766) was deployed at the Lützow-Holm Bay
(LHB) marginal ice zone in Antarctica during the 63rd Japanese Antarctic Research …

We study nonlinear resonant wave–wave interactions which occur when ocean waves
propagate into a thin floating ice sheet. Using multiple-scale perturbation analysis, we obtain …

Commentary narrated in this theme issue is recast to contextualize the diverse themes
presented into a forward-looking conversation that synthesizes, debates opportunities for …

Two drifting wave buoys were deployed in the central Arctic Ocean, north of the Laptev Sea,
where there are historically no wave observations available. An experimental wave buoy …

Sea spray emission is the largest mass flux of aerosols to the atmosphere with important
impact on atmospheric radiative transfer. However, large uncertainties still exit in …