supercooled's Usage Examples:

Droplets of supercooled water often exist in stratus and cumulus clouds.

Icing conditions exist when the air contains droplets of supercooled liquid water; icing conditions are characterized quantitatively by the.

persists in liquid state below this temperature is said to be supercooled, and supercooled water droplets cause icing on aircraft.

hail, hominy snow, or snow pellets, is precipitation that forms when supercooled water droplets are collected and freeze on falling snowflakes, forming.

The raindrops become supercooled while passing through a sub-freezing layer of air hundreds of meters.

Rime ice forms when supercooled water liquid droplets freeze onto surfaces.

visible ice at low temperatures and very low humidity, and rime under supercooled wet conditions.

although these are in a supercooled state.

Ice crystals are the predominant component, and typically, the ice crystals cause the supercooled water drops in the.

condensed matter physics and physical chemistry, the terms viscous liquid, supercooled liquid, and glassforming liquid are often used interchangeably to designate.

of loose, randomly oriented, plate or discoid ice crystals formed in supercooled turbulent water.

persist in a supercooled state, ice nuclei can trigger droplets to freeze.

Contact nucleation can occur if an ice nucleus collides with a supercooled droplet.

This is seen for example in the nucleation of ice in supercooled small water droplets.

The hypothesis was that the silver iodide would cause supercooled water in the storm to freeze, disrupting the inner structure of the hurricane.

temperature is between 0 °C (32 °F) and −3 °C (27 °F) and there are supercooled, relatively large drops of water (from freezing fog).

structure in time approaches an equilibrium density corresponding to the supercooled liquid at this same temperature.

One main type of PSC is made up mostly of supercooled droplets of water and nitric acid and is implicated in the formation.

Dendritic crystals can grow into a supercooled pure liquid or form from growth instabilities that occur when the growth.

Apart from forming from supercooled water, ice Ic has also been reported to form from amorphous ice as well.

When no CCNs are present, water vapour can be supercooled at about −13 °C (8 °F) for 5–6 hours before droplets spontaneously form.

Cumulus clouds can be formed from water vapour, supercooled water droplets, or ice crystals, depending upon the ambient temperature.