Ice Nucleation

Ice nucleation is the process where water molecules begin to organize into a solid ice structure. It typically happens when conditions like temperature and humidity are just right, often around freezing temperatures. Tiny particles or surfaces, called nuclei, help molecules stick together, making it easier for ice to form. Without these nuclei, supercooled water can stay liquid below freezing. Ice nucleation is important in weather patterns, cloud formation, and even in various industrial processes, as it influences when and how ice forms in different environments.