Supercooled water

Research output: Chapter in Book/Report/Conference proceedingEntry for encyclopedia/dictionary

1 Citation (Scopus)

Abstract

Whilst the transition from liquid water to ice is typically considered to occur at 0°C, there are a number of reasons why water can exist in a supercooled liquid state below this freezing point. Furthermore, the existence of supercooled water in the cryosphere has fundamental implications for important phenomena including frost heave of permafrost, glacier motion and dynamics, sea ice formation, the clogging of rivers and hydroelectric power inlets with frazil ice, and the design of power and telecommunications infrastructure and aircraft.

Original languageEnglish
Title of host publicationEncyclopedia of Snow, Ice and Glaciers
EditorsVijay P. Singh, Pratap Singh, Umesh K. Haritashya
PublisherSpringer
Pages1108-1112
Number of pages5
VolumePart 3
ISBN (Electronic)9789048126422
ISBN (Print)9789048126415
DOIs
Publication statusPublished - 26 Aug 2014

Publication series

NameEncyclopedia of Earth Sciences Series
PublisherSpringer Netherlands
ISSN (Print)1388-4360

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  • Cite this

    Cook, S. J. (2014). Supercooled water. In V. P. Singh, P. Singh, & U. K. Haritashya (Eds.), Encyclopedia of Snow, Ice and Glaciers (Vol. Part 3, pp. 1108-1112). (Encyclopedia of Earth Sciences Series). Springer . https://doi.org/10.1007/978-90-481-2642-2_555