Moon Retreats 3.8 Centimeters a Year as Tides Lengthen Earth Days by 2 Milliseconds
Updated
Updated · spacedaily.com · Aug 11
Moon Retreats 3.8 Centimeters a Year as Tides Lengthen Earth Days by 2 Milliseconds
1 articles · Updated · spacedaily.com · Aug 11
Summary
Laser measurements using Apollo mirror arrays show the Moon is receding from Earth by 3.8 centimeters a year, while Earth’s day lengthens by about 2 milliseconds per century.
Tidal friction drives both changes: ocean bulges raised mainly by the Moon sap Earth’s rotational energy, and the offset bulge transfers some of that energy to the Moon’s orbit, pushing it outward.
The arithmetic also explains why lunar tides dominate— the Sun’s tide-generating pull is about 46% of the Moon’s, while all other planets combined are negligible despite occasional alignment scares.
Evidence stretches from Babylonian eclipse records to 620-million-year-old tidal rock bands in South Australia, which indicate Earth once had a 21.9-hour day when the Moon was closer.
That slow orbital trade still matters today: the Moon’s 18.6-year wobble is expected to amplify climate-driven sea-level rise in the mid-2030s, worsening sunny-day flooding.