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    Reply to “Comments on ‘A Wave-Resolving Simulation of Langmuir Circulations with a Nonhydrostatic Free-Surface Model: Comparison with Craik–Leibovich Theory and an Alternative Eulerian View of the Driving Mechanism’”

    Source: Journal of Physical Oceanography:;2019:;volume 049:;issue 003::page 889
    Author:
    Fujiwara, Yasushi
    ,
    Yoshikawa, Yutaka
    ,
    Matsumura, Yoshimasa
    DOI: 10.1175/JPO-D-19-0015.1
    Publisher: American Meteorological Society
    Abstract: AbstractFujiwara et al. explicitly simulated Langmuir circulations using a wave-resolving simulation (WRS) technique and found that the residual wave effect on vorticity was well represented by the vortex force of the Craik?Leibovich (CL) equation, at least in the simulated situation. In response to the simulation results, Mellor has proposed a view that ubiquitous applicability of the CL formulation is still questionable and that the three-dimensional radiation stress (3DRS) formulation that he has derived encompasses both of the vortex force effect and an effect that is lower order in terms of wave steepness. Here, these opinions are discussed in terms of the approximations used in the wave-averaged formulations. The asymptotic expansion of the Eulerian-averaged momentum equation allows the separate discussion of two different wave effects: pressure correction and torque. It is argued that the approximation adopted in Mellor?s 3DRS formulation is presumably not accurate enough to properly parameterize the wave torque effect, and possible approaches to examine its performance are proposed. We agree with the view that the applicability of the CL formulation needs further investigation. WRS will be a helpful tool for this purpose.
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      Reply to “Comments on ‘A Wave-Resolving Simulation of Langmuir Circulations with a Nonhydrostatic Free-Surface Model: Comparison with Craik–Leibovich Theory and an Alternative Eulerian View of the Driving Mechanism’”

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    contributor authorFujiwara, Yasushi
    contributor authorYoshikawa, Yutaka
    contributor authorMatsumura, Yoshimasa
    date accessioned2019-10-05T06:48:35Z
    date available2019-10-05T06:48:35Z
    date copyright3/1/2019 12:00:00 AM
    date issued2019
    identifier otherJPO-D-19-0015.1.pdf
    identifier urihttp://yetl.yabesh.ir/yetl1/handle/yetl/4263484
    description abstractAbstractFujiwara et al. explicitly simulated Langmuir circulations using a wave-resolving simulation (WRS) technique and found that the residual wave effect on vorticity was well represented by the vortex force of the Craik?Leibovich (CL) equation, at least in the simulated situation. In response to the simulation results, Mellor has proposed a view that ubiquitous applicability of the CL formulation is still questionable and that the three-dimensional radiation stress (3DRS) formulation that he has derived encompasses both of the vortex force effect and an effect that is lower order in terms of wave steepness. Here, these opinions are discussed in terms of the approximations used in the wave-averaged formulations. The asymptotic expansion of the Eulerian-averaged momentum equation allows the separate discussion of two different wave effects: pressure correction and torque. It is argued that the approximation adopted in Mellor?s 3DRS formulation is presumably not accurate enough to properly parameterize the wave torque effect, and possible approaches to examine its performance are proposed. We agree with the view that the applicability of the CL formulation needs further investigation. WRS will be a helpful tool for this purpose.
    publisherAmerican Meteorological Society
    titleReply to “Comments on ‘A Wave-Resolving Simulation of Langmuir Circulations with a Nonhydrostatic Free-Surface Model: Comparison with Craik–Leibovich Theory and an Alternative Eulerian View of the Driving Mechanism’”
    typeJournal Paper
    journal volume49
    journal issue3
    journal titleJournal of Physical Oceanography
    identifier doi10.1175/JPO-D-19-0015.1
    journal fristpage889
    journal lastpage892
    treeJournal of Physical Oceanography:;2019:;volume 049:;issue 003
    contenttypeFulltext
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