Ice nucleus

An ice nucleus, also known as an ice nucleating particle (INP), is a particle which acts as the nucleus for the formation of an ice crystal in the atmosphere.

Ice nucleation mechanisms.[clarification needed]


There are a number of mechanisms of ice nucleation in the atmosphere through which ice nuclei can catalyse the formation of ice particles. In the upper troposphere, water vapor can deposit directly onto solid particle. In clouds warmer than about −37 °C where liquid water can persist in a supercooled state, ice nuclei can trigger droplets to freeze.[1]

Contact nucleation can occur if an ice nucleus collides with a supercooled droplet, but the more important mechanism of freezing is when an ice nucleus becomes immersed in a supercooled water droplet and then triggers freezing.

In the absence of an ice nucleating particle, pure water droplets can persist in a supercooled state to temperatures approaching −37 °C where they freeze homogeneously.[2][3][4]

Cloud dynamicsEdit

Ice particles can have a significant effect on cloud dynamics. They are known to be important in the processes by which clouds can become electrified, which causes lightning. They are also known to be able to form the seeds for rain droplets. It has become clear that the concentration of ice nucleating particles in shallow clouds is a key factor in cloud-climate feedbacks.[5][6]

Atmospheric particulate matterEdit

Many different types of atmospheric particulate matter can act as ice nuclei, both natural and anthropogenic, including those composed of desert dust, soot, organic matter, bacteria (e.g. Pseudomonas syringae), pollen, fungal spores and volcanic ash amongst others.[1][7] However, the exact nucleation potential of each type varies greatly, depending on the exact atmospheric conditions. Very little is known about the spatial distribution of these particles, their overall importance for global climate through ice cloud formation, and whether human activity has played a major role in changing these effects.

See alsoEdit


  1. ^ a b Murray; et al. (2012). "Ice nucleation by particles immersed in supercooled cloud droplets". Chem Soc Rev. 41 (19): 6519–6554. doi:10.1039/c2cs35200a. PMID 22932664.
  2. ^ Kulkarni G (2014). "Ice nucleation of bare and sulfuric acid-coated mineral dust particles and implication for cloud properties". Journal of Geophysical Research. 119 (16): 9993–10011. Bibcode:2014JGRD..119.9993K. doi:10.1002/2014JD021567.
  3. ^ Koop, T. (March 25, 2004). "Homogeneous ice nucleation in water and aqueous solutions". Zeitschrift für Physikalische Chemie. 218 (11): 1231–1258. doi:10.1524/zpch.218.11.1231.50812. S2CID 46915879. Retrieved 2008-04-07.
  4. ^ Murray B (2010). "Homogeneous ice nucleation in water and aqueous solutions". Physical Chemistry Chemical Physics. 12 (35): 10380–10387. Bibcode:2010PCCP...1210380M. doi:10.1039/c003297b. PMID 20577704.
  5. ^ Murray, Benjamin J.; Carslaw, Kenneth S.; Field, Paul R. (21 August 2020). "Opinion: Cloud-phase climate feedback and the importance of ice-nucleating particles". doi:10.5194/acp-2020-852. Cite journal requires |journal= (help)
  6. ^ Vergara-Temprado, Jesús; Miltenberger, Annette K.; Furtado, Kalli; Grosvenor, Daniel P.; Shipway, Ben J.; Hill, Adrian A.; Wilkinson, Jonathan M.; Field, Paul R.; Murray, Benjamin J.; Carslaw, Ken S. (13 March 2018). "Strong control of Southern Ocean cloud reflectivity by ice-nucleating particles". Proceedings of the National Academy of Sciences. 115 (11): 2687–2692. Bibcode:2018PNAS..115.2687V. doi:10.1073/pnas.1721627115. PMC 5856555. PMID 29490918.
  7. ^ Christner BC, Morris CE, Foreman CM, Cai R, Sands DC (2008). "Ubiquity of biological ice nucleators in snowfall". Science. 319 (5867): 1214. Bibcode:2008Sci...319.1214C. CiteSeerX doi:10.1126/science.1149757. PMID 18309078. S2CID 39398426.