Other planets, dwarf planets, and moons in our solar system have seasonal cycles that differ from Earth's due to factors like axial tilt and orbit shape.
For example, Mars has an axial tilt of around 25 degrees, resulting in seasonal variations similar to Earth, with winters dominated by carbon dioxide ice.
Planets like Mercury, with no tilt, experience minimal seasonal changes, while Uranus, with a 90-degree tilt, has intense and extreme seasons.
The tilt and shape of a planet's orbit can impact seasonal changes, with variations seen over billions of years, influencing planetary conditions and potential for life.