10 likes | 134 Vues
The Milankovitch Theory explains how the Earth's orbital changes—eccentricity, axial precession, and obliquity—affect climate patterns over geological time scales. These factors influence the distribution and intensity of sunlight received on Earth, leading to cycles of glacial and interglacial periods. Understanding these natural processes is crucial in the context of global warming debates, as they provide insight into historical climate changes, helping to discern the differences between natural climate variability and anthropogenic influences on modern climate change.
E N D