In contrast to cloud condensation nuclei, the most
effective ice nuclei are hydrophobic (having a low affinity for water) with molecular spacings and a crystallographic structure close to that of ice.
Ice crystal nucleation is a whole other thing... (some aerosols are more
effective ice nuclei than others.
The vapor pressure in equilibrium with supercooled droplets (liquid H2O) is higher than that in equilibrium with solid H2O at the same temperature, so liquid droplets will evaporate to feed deposition on
an effective ice nucleus.
Not exact matches
Aerosols that are
effective for the conversion of water vapour to
ice crystals are referred to as
ice nuclei.
In a process called cloud seeding, silver iodide, with
effective ice - nucleating temperatures of less than − 4 °C, has been used for years in attempts to convert supercooled water to
ice crystals in regions with a scarcity of natural
ice nuclei.
The underlying mechanism is that charged aerosols are more
effective than neutral aerosols as
ice nuclei (i.e., electrofreezing) and that the enhanced collections of charged evaporation
nuclei by supercooled droplets enhance the production of
ice by contact
ice nucleation (i.e., electroscavenging).