
Water that remains liquid below its freezing point until disturbed, then rapidly freezes.Supercooled water is liquid water that has been cooled below its normal freezing point of 0°C (32°F) without turning into ice. This is a metastable state: the water is poised on the edge of freezing, but as long as it is undisturbed and free of impurities, it can remain liquid at temperatures as low as -40°C or even lower. The phenomenon occurs because freezing requires nucleation — a tiny seed of ice crystal to start the process. Without such a seed, the water molecules lack a template to arrange into a crystalline structure, so they continue to jostle about in a liquid state despite the low temperature.
The phenomenon was first systematically studied in the 18th century, with early experiments by Johann Heinrich Lambert and others demonstrating that water could be cooled below freezing without solidifying. The term 'supercooling' was coined later, and the modern understanding of nucleation was developed in the 20th century through the work of physicists like Richard Becker and Werner Döring.
When water cools below 0°C, the molecules slow down and their hydrogen bonds begin to align into a tetrahedral network, which is the structure of ice. However, this alignment is a cooperative process that needs a starting point. In pure water, random thermal fluctuations can occasionally create a small cluster of ice-like structure, but if the cluster is too small, it dissolves again. Only when a cluster reaches a critical size — typically a few hundred molecules — does it become stable and grow into ice. This critical nucleus is unlikely to form spontaneously in clean, quiescent water, so the water remains liquid. Disturbing the water, such as shaking it or dropping a small ice crystal into it, provides the necessary nucleation site, triggering rapid freezing throughout the entire volume.
Supercooling is used in cryopreservation techniques to protect biological cells from ice damage during freezing, as well as in cloud seeding research to understand how ice forms in the atmosphere.
A supercooled water droplet can freeze almost instantly when touched by a single ice crystal, forming a dramatic 'ice spike' as the freezing front races through the liquid.










