Wave Boundary Layer at the Ice–Water Interface

On re-examining the problem of linear gravity waves in two layers of fluids with a viscous ice layer overlaying water of deep depth, we give a detailed analysis of the fluid velocities, velocity shear, and Reynolds stress associated with wave fluctuations in both the ice layer and the wave boundary...

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Main Author: Jie Yu
Format: Article
Language:English
Published: MDPI AG 2022-10-01
Series:Journal of Marine Science and Engineering
Subjects:
Online Access:https://www.mdpi.com/2077-1312/10/10/1472
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author Jie Yu
author_facet Jie Yu
author_sort Jie Yu
collection DOAJ
description On re-examining the problem of linear gravity waves in two layers of fluids with a viscous ice layer overlaying water of deep depth, we give a detailed analysis of the fluid velocities, velocity shear, and Reynolds stress associated with wave fluctuations in both the ice layer and the wave boundary layer just beneath it. For the turbulent wave boundary layer, water eddy viscosity is used. Comprehensive discussions on various aspects of the velocity fields are made in terms of a Reynolds number based on the ice-layer thickness and viscosity, and the ice-to-water viscosity ratio. Speculation of the wave-induced steady streaming is made based on the Reynolds stress distribution, offering a preliminary insight into the mean flows in both the ice layer and wave boundary layer in the water. For wave attenuation, the results using a typical ice viscosity and a reasonable water eddy viscosity show good agreement with data over the range of frequencies for field and lab waves, significantly outperforming those assuming an inviscid water.
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spelling doaj.art-a035c8086cf6488d911196833a64a73e2023-11-24T00:44:45ZengMDPI AGJournal of Marine Science and Engineering2077-13122022-10-011010147210.3390/jmse10101472Wave Boundary Layer at the Ice–Water InterfaceJie Yu0Naval Research Laboratory, Stennis Space Center, MS 39529, USAOn re-examining the problem of linear gravity waves in two layers of fluids with a viscous ice layer overlaying water of deep depth, we give a detailed analysis of the fluid velocities, velocity shear, and Reynolds stress associated with wave fluctuations in both the ice layer and the wave boundary layer just beneath it. For the turbulent wave boundary layer, water eddy viscosity is used. Comprehensive discussions on various aspects of the velocity fields are made in terms of a Reynolds number based on the ice-layer thickness and viscosity, and the ice-to-water viscosity ratio. Speculation of the wave-induced steady streaming is made based on the Reynolds stress distribution, offering a preliminary insight into the mean flows in both the ice layer and wave boundary layer in the water. For wave attenuation, the results using a typical ice viscosity and a reasonable water eddy viscosity show good agreement with data over the range of frequencies for field and lab waves, significantly outperforming those assuming an inviscid water.https://www.mdpi.com/2077-1312/10/10/1472wave boundary layer under icemarginal ice zonewave-induced Reynolds stresssteady streaming
spellingShingle Jie Yu
Wave Boundary Layer at the Ice–Water Interface
Journal of Marine Science and Engineering
wave boundary layer under ice
marginal ice zone
wave-induced Reynolds stress
steady streaming
title Wave Boundary Layer at the Ice–Water Interface
title_full Wave Boundary Layer at the Ice–Water Interface
title_fullStr Wave Boundary Layer at the Ice–Water Interface
title_full_unstemmed Wave Boundary Layer at the Ice–Water Interface
title_short Wave Boundary Layer at the Ice–Water Interface
title_sort wave boundary layer at the ice water interface
topic wave boundary layer under ice
marginal ice zone
wave-induced Reynolds stress
steady streaming
url https://www.mdpi.com/2077-1312/10/10/1472
work_keys_str_mv AT jieyu waveboundarylayerattheicewaterinterface