The Milankovitch cycle refers to the variations in the Earth's orbital and axial movements that influence the planet's climate. These cycles are also known as Milankovitch parameters or astronomical cycles. Other synonyms for Milankovitch cycle include Orbital forcing theory, Astronomical forcing theory, and Paleoclimatic cycles. These synonyms are used interchangeably to describe the same phenomenon through various scientific disciplines. Understanding the Milankovitch cycle is critical to understanding the long-term climate history of the planet, as well as predicting future climate changes. Overall, the synonyms for Milankovitch cycle help to deepen our knowledge and understanding of how the Earth's climate has changed over time and how it may continue to change in the future.