Transient Shallow Water Wave Interactions with a Partially Fragmented Ice Shelf

This work investigates the interaction between water waves and multiple ice shelf fragments in front of a semi-infinite ice sheet. The hydrodynamics are modelled using shallow water wave theory and the ice shelf vibration is modelled using Euler–Bernoulli beam theory. The ensuing multiple scattering problem is solved in the frequency domain using the transfer matrix method. The appropriate conservation of energy identity is derived in order to validate our numerical calculations. The transient scattering problem for incident wave packets is constructed from the frequency domain solutions. By incorporating multiple scattering, this paper extends previous models that have only considered a continuous semi-infinite ice shelf. This paper serves as a fundamental step towards developing a comprehensive model to simulate the breakup of ice shelves.

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Publication Details

Journal
Fluids
Published
2024-08-21
DOI
https://doi.org/10.3390/fluids9080192
Citations
2
Primary Topic
Cryospheric studies and observations
Type
article
Field-Weighted Citation Impact
0.75

Funders

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article

Transient Shallow Water Wave Interactions with a Partially Fragmented Ice Shelf

Ben Wilks, Michael Howard Meylan, Faraj Alshahrani
2 citations
Fluids
Cryospheric studies and observations
0.75
article

Transient Shallow Water Wave Interactions with a Partially Fragmented Ice Shelf

Ben Wilks, Michael Howard Meylan, Faraj Alshahrani
article en
2 citations

Abstract

This work investigates the interaction between water waves and multiple ice shelf fragments in front of a semi-infinite ice sheet. The hydrodynamics are modelled using shallow water wave theory and the ice shelf vibration is modelled using Euler–Bernoulli beam theory. The ensuing multiple scattering problem is solved in the frequency domain using the transfer matrix method. The appropriate conservation of energy identity is derived in order to validate our numerical calculations. The transient scattering problem for incident wave packets is constructed from the frequency domain solutions. By incorporating multiple scattering, this paper extends previous models that have only considered a continuous semi-infinite ice shelf. This paper serves as a fundamental step towards developing a comprehensive model to simulate the breakup of ice shelves.

FluidsVol. 9(8)
Prince Sattam Bin Abdulaziz University (SA), University of Newcastle Australia (AU)
Australian Government
Openalex Percentile: Top 31%
Cryospheric studies and observations
0.75
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Transient Shallow Water Wave Interactions with a Partially Fragmented Ice Shelf — Ben Wilks, Michael Howard Meylan, et al. · Fluids (2024) | TGRS Research Map | TGRS