Wave Attenuation Through an Arctic Marginal Ice Zone on 12 October 2015: 1. Measurement of Wave Spectra and Ice Features From Sentinel 1A

• Published in: Journal of Geophysical Research: Oceans
• Main Authors: Stopa, J. E., Ardhuin, Fabrice, Thomson, Jim, Smith, Madison M., Kohout, Alison, Doble, Martin, Wadhams, Peter
• Other Authors: Institut Français de Recherche pour l'Exploitation de la Mer (IFREMER), Université de Brest (UBO), Laboratoire d'Océanographie Spatiale (LOS), University at Albany SUNY, State University of New York (SUNY), EU-FP7 project SWARP 607476, ONROffice of Naval Research N0001416WX01117, CNESCentre National D'etudes Spatiales, LabexMer ANR-10-LABX-19-01, NSFNational Science Foundation (NSF)
• Format: Article in Journal/Newspaper
• Language: English
• Published: HAL CCSD 2018
• Subjects: wave-ice interaction; Arctic Ocean marginal ice zone; Sentinel-1A SAR; Arctic Sea State Boundary Layer Physics Program; remote sensing; wave attenuation; [SDV.MP]Life Sciences [q-bio]/Microbiology and Parasitology; Arctic; Arctic Ocean; Beaufort Sea; Sea ice
• Online Access: https://hal.archives-ouvertes.fr/hal-02929085; https://doi.org/10.1029/2018JC013791

A storm with significant wave heights exceeding 4 m occurred in the Beaufort Sea on 11-13 October 2015. The waves and ice were captured on 12 October by the Synthetic Aperture Radar (SAR) on board Sentinel-1A, with Interferometric Wide swath images covering 400 x 1,100 km at 10 m resolution. This data set allows the estimation of wave spectra across the marginal ice zone (MIZ) every 5 km, over 400 km of sea ice. Since ice attenuates waves with wavelengths shorter than 50 m in a few kilometers, the longer waves are clearly imaged by SAR in sea ice. Obtaining wave spectra from the image requires a careful estimation of the blurring effect produced by unresolved wavelengths in the azimuthal direction. Using in situ wave buoy measurements as reference, we establish that this azimuth cutoff can be estimated in mixed ocean-ice conditions. Wave spectra could not be estimated where ice features such as leads contribute to a large fraction of the radar backscatter variance. The resulting wave height map exhibits a steep decay in the first 100 km of ice, with a transition into a weaker decay further away. This unique wave decay pattern transitions where large-scale ice features such as leads become visible. As in situ ice information is limited, it is not known whether the decay is caused by a difference in ice properties or a wave dissipation mechanism. The implications of the observed wave patterns are discussed in the context of other observations. Plain Language Summary Our work entitled Wave attenuation through an Arctic marginal ice zone on 12 October 2015. 1. Measurement of wave spectra and ice features from Sentinel-1A, uses a newly developed method to extract wave spectra from radar imagery over sea ice. This is possible since the sea ice rapidly removes the short waves which usually distort the radar imagery. We are able to estimate thousands of wave spectra across several hundred kilometers at kilometer-scale resolution for the first large-scale view of wave attenuation across the marginal ice zone. Our results ...