Ice crystals can also grow when
supercooled water freezes directly onto the crystal to form rime.
rime ice A coating of tiny, opaque ice crystals formed when
supercooled water freezes rapidly on contact with an object.
Not exact matches
Supercooled water droplets in a cloud can remain liquid at temperatures far below
freezing, their surface tension preventing solid crystals from forming.
The extremely low temperatures and rapid
freezing were crucial to forming cubic ice, Wyslouzil said: «Since liquid
water drops in high - altitude clouds are typically
supercooled, there is a good chance for cubic ice to form there.»
In winter the observers didn't use the anemometer, an instrument for measuring wind speed, for fear it would be damaged by the
supercooled water droplets that
froze to everything, leaving the observatory caked in windblown ice.
Without the presence of these impurities, however, the
water can be
supercooled past its
freezing point.
Water also refreezes when it is forced up valley walls, experiencing a rapid change in pressure that triggers a
freezing process known as «
supercooling.»
Supercooled water - below
freezing but still a liquid - is notoriously difficult to study.
It is possible to keep the ice from
freezing (
supercooled), if you use distilled
water and are very careful about the container and not jiggling it, etc..
Eventually, when a temperature of about -10 °C is reached, the
water droplets of the cloud (which are by then
supercooled) begin to
freeze and become ice crystals.
Contact and
freezing nuclei, in contrast, are associated with the conversion of
supercooled water to ice.
Freezing nuclei are absorbed into the liquid
water and convert the
supercooled water to ice from the inside out.
In the absence of any ice nuclei, the
freezing of
supercooled water droplets of a few micrometres in radius, in a process called homogeneous ice nucleation, requires temperatures at or lower than − 39 °C (− 38 °F).