Milankovitch Cycles

Milankovitch Cycles refer to the long-term changes in Earth's orbit and axial tilt that affect its climate over thousands of years. These cycles include variations in the shape of Earth's orbit (eccentricity), the tilt of its axis (obliquity), and the wobble of its axis (precession). These factors influence the distribution and intensity of sunlight reaching Earth, contributing to the timing of ice ages and warm periods. Understanding these cycles helps explain natural climate changes and how they relate to our planet's geological history.