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mean diurnal low-water inequality |
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mean diurnal low-water inequality [′mēn dī′ərn·əl ′lō ‚wȯd·ər ‚in·i·′kwal·əd·ē]
(oceanography) Half the average difference between the heights of the two low waters of each tidal day over a 19-year period; it is obtained by subtracting the mean of all lower low waters from the mean of the low waters. Want to thank TFD for its existence? Tell a friend about us, add a link to this page, add the site to iGoogle, or visit the webmaster's page for free fun content. |
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