In order to gauge the extent to which wave-mean interactions may be significant, it is convenient to evaluate the ratio of time scales characterizing wave-wave and wave-mean interactions.
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Assessment of fine-scale parameterizations at low latitudes of the North Pacific.
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The sentences
ε MG show a decreasing trend with increasing depth as ε OB while ε GHP trend to slightly increase with increasing depth below 500 m where ε GHP deviate from the observed values.