Answer:
Besides that, the surface heating is uneven. Much more heat is absorbed in low than at high latitudes. This is because the Earth's surface gradually tilts away from the sun (the sun is lower on the horizon) as you move away from the equator.
Explanation:
As obliquity decreases, it gradually helps make our seasons milder, resulting in increasingly warmer winters, and cooler summers that gradually, over time, allow snow and ice at high latitudes to build up into large ice sheets.
