તે ખૂબ ઠંડી છે,

supercooled's Usage Examples:

Recalescence also occurs after supercooling, when the supercooled liquid suddenly crystallizes, forming a solid but.

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

in which the water is not supercooled and for a glacier far into the supercooling regime vary significantly.

masses by attracting supercooled cloud water droplets, which freeze and accrete in crystal form.

quantum electrodynamics, the physics of the superfluidity of supercooled liquid helium, as well as his work in particle physics for which he proposed the.

appearance of a crystalline phase from either a supercooled liquid or a supersaturated solvent.

snow, or snow pellets, is precipitation that forms when supercooled water droplets are collected and freeze on falling snowflakes, forming 2–5 mm (0.

although these are in a supercooled state.

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

According to Bergeron, most precipitation is formed as a consequence of water evaporating from small supercooled droplets and accreting onto ice crystals, which then fall as snow, or melt and fall as cold rain depending on the ambient air temperature.

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

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

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