The reference tide is the hypothetical constituent " equilibrium tide " on a landless Earth measured at 0?longitude, the Greenwich meridian.
2.
Earth's " net " ( or " equivalent " ) equilibrium tide has an amplitude of only 3.23 cm, which is totally swamped by oceanic tides that can exceed one metre.
3.
The Love number "'h "'is defined as the ratio of the body tide to the height of the static equilibrium tide; also defined as the vertical ( radial ) displacement or variation of the planet's elastic properties.
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