Direct in-situ observations of wave-induced floe collisions in the deeper Marginal Ice Zone

Fuente: arXiv
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Auteurs principaux: Dreyer, Lars Willas, Rabault, Jean, Jensen, Atle, Dæhlen, Ingrid, Breivik, Øyvind, Hope, Gaute, Kristoffersen, Yngve
Format: Preprint
Publié: 2024
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author Dreyer, Lars Willas
Rabault, Jean
Jensen, Atle
Dæhlen, Ingrid
Breivik, Øyvind
Hope, Gaute
Kristoffersen, Yngve
author_facet Dreyer, Lars Willas
Rabault, Jean
Jensen, Atle
Dæhlen, Ingrid
Breivik, Øyvind
Hope, Gaute
Kristoffersen, Yngve
contents Ocean waves propagating through the Marginal Ice Zone (MIZ) and the pack ice are strongly attenuated. This attenuation is critical for protecting sea ice from energetic wave events that could otherwise lead to sea ice break-up and dislocation over large areas. Despite the importance of waves-in-ice attenuation, the exact physical mechanisms involved, and their relative importance, are still uncertain. Here we present direct in situ measurements of floe-floe interactions under the influence of waves, including collisions between adjacent floes. The collision events we report are aligned with the incoming wave direction, and phase-locked to the wave signal, which indicates that the individual collisions we detect are wave-induced. The observations indicate a possible correlation between sudden increases in wave activity and the frequency of floe-floe collisions
format Preprint
id arxiv_https___arxiv_org_abs_2404_02750
institution arXiv
publishDate 2024
record_format arxiv
spellingShingle Direct in-situ observations of wave-induced floe collisions in the deeper Marginal Ice Zone
Dreyer, Lars Willas
Rabault, Jean
Jensen, Atle
Dæhlen, Ingrid
Breivik, Øyvind
Hope, Gaute
Kristoffersen, Yngve
Atmospheric and Oceanic Physics
Ocean waves propagating through the Marginal Ice Zone (MIZ) and the pack ice are strongly attenuated. This attenuation is critical for protecting sea ice from energetic wave events that could otherwise lead to sea ice break-up and dislocation over large areas. Despite the importance of waves-in-ice attenuation, the exact physical mechanisms involved, and their relative importance, are still uncertain. Here we present direct in situ measurements of floe-floe interactions under the influence of waves, including collisions between adjacent floes. The collision events we report are aligned with the incoming wave direction, and phase-locked to the wave signal, which indicates that the individual collisions we detect are wave-induced. The observations indicate a possible correlation between sudden increases in wave activity and the frequency of floe-floe collisions
title Direct in-situ observations of wave-induced floe collisions in the deeper Marginal Ice Zone
topic Atmospheric and Oceanic Physics
url https://arxiv.org/abs/2404.02750