Wave dispersion and dissipation in landfast ice: comparison of observations against models

Abstract

Abstract. Observations of wave dissipation and dispersion in sea ice are a necessity for the development and validation of wave-ice interaction models. As the composition of the ice layer can be extremely complex, most models treat the ice layer as a continuum with effective, rather than independently measurable, properties. While this provides opportunities to fit the model to observations, it also obscures our understanding of the wave-ice interactive processes, particularly, it hinders our ability to identify under which environmental conditions these processes are of significance. Here, we aimed to reduce the number of free variables available by studying wave dissipation in landfast ice. That is, in continuous sea ice, such as landfast ice, the effective properties of the continuum ice layer should revert to the material properties of the ice. We present observations of wave dispersion and dissipation from a field experiment on landfast ice in the Arctic and Antarctic. Independent laboratory measurements were performed on sea ice cores from a neighbouring fjord in the Arctic to estimate the ice viscosity. Results show that the dispersion of waves in landfast ice is well described by theory of a thin elastic plate and such observations could provide an estimate of the elastic modulus of the ice. Observations of wave dissipation in landfast ice are about an order of magnitude larger than in ice floes and broken ice. Comparison of our observations against models suggests that wave dissipation is attributed to the viscous dissipation within the ice layer for short waves only, whereas turbulence generated through the interactions between the ice and waves is the most likely process for the dissipation of wave energy for long periods. The separation between short and long waves in this context is expected to be determined by the ice thickness through its influence on the lengthening of short waves. Further studies are required to measure turbulence underneath the ice independently of observations of wave attenuation to confirm our interpretation of the results.

Wave-in-ice: theoretical bases and field observations

“…Voermans et al . [57] compared several viscoelastic and basal friction models with data obtained in landfast ice. It was found that for short waves viscoelastic effects dominated and for long waves basal friction dominated.…”

“…Many of these studies focused on pancake ice or broken ice fields [52–55]. A few also investigated grease ice [56] and landfast ice [57]. Most of these studies addressed wave attenuation, with a few included wave speed [51,57–59].…”

“…A few also investigated grease ice [56] and landfast ice [57]. Most of these studies addressed wave attenuation, with a few included wave speed [51,57–59]. Early laboratory studies have been reviewed in [8].…”

A Two‐Part Model for Wave‐Sea Ice Interaction: Attenuation and Break‐Up

“…A conservative range for Y and σ was chosen to describe the full range of sea ice material properties, with σ ∈[0.1, 0.7] MPa and Y ∈[0.2, 9] GPa (Karulina et al., 2019; Timco & Weeks, 2010). The range for the attenuation reduction coefficient for broken ice is β ∈[0.01, 0.1] (Voermans et al., 2021). Here, we choose β = 0.05 as being the median value.…”

“…Both report two distinct phases in attenuation of waves by sea ice: strong attenuation under unbroken ice conditions, and unimpeded propagation under broken ice conditions. Wave attenuation reduces by at least an order of magnitude once the ice is broken (Voermans et al., 2021), hence the waves can propagate further and break more sea ice.…”