Reply to “Comments on ‘Langmuir Turbulence and Surface Heating in the Ocean Surface Boundary Layer’”
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AbstractThe differences between the conclusions of Noh and Choi and of Pearson et al., which are largely a result of defining different length scales based on different quantities, are discussed. This study shows that the layer over which Langmuir turbulence mixes (nominally hTKE) under a stabilizing surface buoyancy flux should be scaled by a combination of the Langmuir stability length LL and initial/nocturnal boundary layer depth h0 rather than by the Zilitinkevich length.
2018 ◽
Vol 48
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pp. 455-458
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2017 ◽
Vol 47
(12)
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pp. 2863-2886
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2014 ◽
Vol 119
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pp. 1899-1910
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2009 ◽
Vol 39
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pp. 1077-1096
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2018 ◽
Vol 48
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pp. 1921-1940
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2015 ◽
Vol 45
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pp. 2897-2911
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2021 ◽
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2019 ◽
Vol 49
(11)
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pp. 2935-2959
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