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Flexural-gravity waves in ice channel with a lead

Published online by Cambridge University Press:  28 June 2021

L.D. Zeng Open the ORCID record for L.D. Zeng [Opens in a new window] ,
A.A. Korobkin ,
B.Y. Ni  and
Y.Z. Xue
L.D. Zeng
Affiliation:
College of Shipbuilding Engineering, Harbin Engineering University, Harbin 150001, PR China
A.A. Korobkin*
Affiliation:
School of Mathematics, University of East Anglia, Norwich NR4 7TJ, United Kingdom
B.Y. Ni
Affiliation:
College of Shipbuilding Engineering, Harbin Engineering University, Harbin 150001, PR China
Y.Z. Xue
Affiliation:
College of Shipbuilding Engineering, Harbin Engineering University, Harbin 150001, PR China
*
†Email address for correspondence: a.korobkin@uea.ac.uk
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Abstract

The flexural-gravity symmetric waves propagating in an ice channel with a lead of open water in the ice cover are investigated within the linear theory of hydroelasticity. The ice sheets are modelled as either elastic or as rigid plates. Deflections of the elastic ice sheets are described by the linear elastic plate equation. The flexural-gravity waves propagating along the channel and their dispersion relations are obtained by the normal mode method. It is shown that the dispersion relations for elastic ice approach the dispersion relations for rigid ice as the rigidity of ice increases or the wavelength decreases. The region in the plane ice thickness/wavenumber, where the ice cover can be treated as rigid with a prescribed accuracy, is determined. The effects of the ice thickness and width of the lead on the phase speeds are studied to determine critical speeds of a vehicle moving along the channel. It is shown that wave modes have several critical speeds, which may merge for some parameters of the channel. The presence of the lead significantly changes the characteristics of waves in an ice channel. Short waves, which propagate in a channel fully covered with ice, weakly depend on gravity and the presence of water in the channel. However, short waves propagating in the same channel but with a lead of open water are gravity-dominated waves localised in the lead. We conclude that flexural-gravity waves in an ice channel with a lead are less pronounced than in the channel completely covered by ice.

JFM classification

Geophysical and Geological Flows: Ice sheets Waves/Free-surface Flows: Channel flow Waves/Free-surface Flows: Wave-structure interactions

Information

Type
JFM Papers
Information
Journal of Fluid Mechanics , Volume 921 , 25 August 2021 , A10
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Copyright
© The Author(s), 2021. Published by Cambridge University Press

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