Abstract Analysis of field measurements of ocean surface wave activity in the marginal ice zone, from campaigns in the Arctic and Antarctic and over a range of different ice conditions …
WE Rogers, J Thomson, HH Shen… - Journal of …, 2016 - Wiley Online Library
A model for wind‐generated surface gravity waves, WAVEWATCH III®, is used to analyze and interpret buoy measurements of wave spectra. The model is applied to a hindcast of a …
F Collard, L Marié, F Nouguier… - Journal of …, 2022 - Wiley Online Library
Wind‐generated waves strongly interact with sea ice and impact air‐sea exchanges, operations at sea, and marine life. Unfortunately, the dissipation of wave energy is not well …
A large collaborative program has studied the coupled air‐ice‐ocean‐wave processes occurring in the Arctic during the autumn ice advance. The program included a field …
The Arctic marginal ice zone (MIZ), where strong interactions between sea ice, ocean and atmosphere take place, is expanding as the result of ongoing sea ice retreat. Yet, state-of …
Sea ice inhibits the development of wind‐generated surface gravity waves which are the dominant factor in upper ocean mixing and air‐sea fluxes. In turn, sea ice properties are …
The dissipation of wave energy in the marginal ice zone is often attributed to wave scattering and the dissipative mechanisms associated with the ice layer. In this study we present …
WE Rogers, MH Meylan, AL Kohout - Cold Regions Science and …, 2021 - Elsevier
A model-data inversion is applied to an extensive observational dataset collected in the Southern Ocean north of the Ross Sea during late autumn to early winter, producing …
Sea ice is highly complex due to the inhomogeneity of the physical properties (eg temperature and salinity) as well as the permeability and mixture of water and a matrix of …