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Assess the link between local sea-ice drift velocity and floe–floe collision occurrence

Ascertain whether a robust relationship exists between the local sea-ice drift velocity of an individual floe (as measured by 1 Hz GPS during 20-minute intervals) and the presence or absence of wave-induced floe–floe collision events detected in inertial motion unit acceleration data in the Marginal Ice Zone.

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Background

The authors analyze their buoy’s 1 Hz GPS drift data alongside identified collision events, testing for a simple correlation between drift velocity and collision occurrence. Their dataset does not reveal a clear relation, suggesting that either the correlation is weak or non-local, or that larger datasets are needed.

They propose that larger-scale ice-sheet properties (e.g., convergence/divergence patterns) may modulate collisions, but emphasize that further data and analysis are required to evaluate this hypothesis and clarify drivers of collision occurrence.

References

There also, we were not able to find a particular pattern or relation between the sea ice drift velocity at the location of the buoy by itself, and the presence or absence of collisions.

Direct in-situ observations of wave-induced floe collisions in the deeper Marginal Ice Zone (2404.02750 - Dreyer et al., 3 Apr 2024) in Section 4 (Discussion)