Universal discontinuous percolation transition in the Earth's terrestrial topography

Based on the Topographic Wetness Index (TWI), we studied the percolation process of water on the Earth’s land surface and discovered a universal discontinuous phase transition across scales, with a critical TWI threshold of 0.671 (0.054). The discontinuity is attributed to the long-range correlation and directionality of the percolation process. Furthermore, the criticality is shown to extend from the critical point to a region corresponding to the Griffiths phase, where natural lake systems are found to develop, indicating the governess of self-organized criticality within the Earth system.