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mean diurnal high-water inequality

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mean diurnal high-water inequality [′mēn dī′ərn·əl ′hī ‚wȯd·ər ‚in·i′kwäl·əd·ē]
(oceanography)
Half the average difference between the heights of the two high waters of each tidal day over a 19-year period; it is obtained by subtracting the mean of all high waters from the mean of the higher high waters.


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