Frost flower (sea ice)

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This article is about formations on sea ice and lake ice. For extrusions formed on freezing plants, see frost flower.
Frost flowers growing on young sea ice in the Arctic

Frost flowers are ice crystals commonly found growing on young sea ice and thin lake ice in cold, calm conditions. The ice crystals are similar to hoar frost, and are commonly seen to grow in patches around 3–4 cm in diameter. Frost flowers growing on sea ice have extremely high salinities and concentrations of other sea water chemicals and, because of their high surface area, are efficient releasers of these chemicals into the atmosphere.[1][2][3]


Frost flowers are formed on thin sea ice when the atmosphere is much colder than the underlying ice. Typically a temperature difference between the ice surface and the air of at least 15°C is required, though this can be reduced if the air is very humid. In these conditions a layer of supersaturated vapour is found directly above the sea ice, caused by the sublimation of ice into the dry, cold air. As the warmer, wet air meets the overlying cold air it becomes supersaturated and can condense as hoar-frost like crystals on the sea ice surface. In general, frost flowers only form in relatively windless conditions; in high winds the supersaturated layer is scrubbed from the surface and blowing snow obscures the ice surface.[4]

On lake ice, frost flowers are effectively identical to hoar frost crystals. On sea ice, brine is wicked up onto the hoar frost crystals, which leads to high salinities of up to 100psu (ppt) (approximately three times more salty than sea water).[5]

Frost flowers are most commonly found on young sea ice in polar regions as the large temperature differences between the ice and air are suitable for growth. When the ice grows too thick, the upper surface of the ice cools down and frost flowers no longer grow. This means that frost flowers typically only grow in the first few days of ice coverage.[citation needed]


The ice crystals in frost flowers are usually dendritic but similarly to hoar frost can grow in rod-like morphologies. When warm brine is wicked up onto the ice crystals, it can also give the frost flower a 'clumped' appearance as the facets of the ice crystals are partly melted.[6]

Aerosol release[edit]

Frost flowers have attracted interest as a possible source of polar atmospheric aerosol. High chemical concentrations and the extended surface area may facilitate efficient release into the atmosphere. In particular studies have shown that abundance of frost flowers can be linked to high concentrations of tropospheric bromine monoxide causing tropospheric ozone depletion events, and higher quantities of airborne sea-salt particles.[7]

See also[edit]


  1. ^ "Mystery of frost flower growth explained - environment". New Scientist. 20 May 2009. Retrieved 2010-03-28. 
  2. ^ "University of Leeds - Christmassy frost flowers - or symbols of climate change?". 2009-12-17. Retrieved 2010-03-28. 
  3. ^ Roscoe, H. K.; Brooks, B.; Jackson, A. V.; Smith, M. H.; Walker, S. J.; Obbard, R. W.; Wolff, E. W. (2011). "Frost flowers in the laboratory: Growth, characteristics, aerosol, and the underlying sea ice". Journal of Geophysical Research 116. doi:10.1029/2010JD015144.  edit
  4. ^ Style, R. W.; Worster, M. G. (2009). "Frost flower formation on sea ice and lake ice" (PDF). Geophysical Research Letters 36 (11). doi:10.1029/2009GL037304.  edit.
  5. ^ Martin, S.; Drucker, R.; Fort, M. (1995). "A laboratory study of frost flower growth on the surface of young sea ice". Journal of Geophysical Research 100: 7027. doi:10.1029/94JC03243.  edit
  6. ^ Perovich, D. K.; Richter-Menge, J. A. (1994). "Surface characteristics of lead ice" (PDF). Journal of Geophysical Research 99: 16341. doi:10.1029/94JC01194.  edit
  7. ^ Kaleschke, L.; Richter, A.; Burrows, J.; Afe, O.; Heygster, G.; Notholt, J.; Rankin, A. M.; Roscoe, H. K.; Hollwedel, J.; Wagner, T.; Jacobi, H.-W. (2004). "Frost flowers on sea ice as a source of sea salt and their influence on tropospheric halogen chemistry" (PDF). Geophysical Research Letters 31 (16). doi:10.1029/2004GL020655.  edit