That’s where obliquity — the amount of tilting between a planet’s axis and its orbit — comes in, according to Yale astronomers Sarah Millholland and Gregory Laughlin.
“When planets such as these have large axial tilts, as opposed to little or no tilt, their tides are exceedingly more efficient at draining orbital energy into heat in the planets,” said first author Millholland, .... “This vigorous tidal dissipation pries the orbits apart.”
A similar, but not identical, situation exists between Earth and its moon. The moon’s orbit is slowly growing due to dissipation from tides, but Earth’s day is gradually lengthening.
“It impacts several of their physical
features, such as their climate, weather, and global circulations,”
Laughlin said. “The seasons on a planet with a large axial tilt are much
more extreme than those on a well-aligned planet, and their weather
patterns are probably non-trivial.” AstroBiology