Clear ice

Clear ice's theme is one that has captured people's attention for a long time. With its impact on different aspects of life, Clear ice has been the subject of study, debate and discussion in various contexts. Throughout history, Clear ice has played a crucial role in society, culture, and human development. As we continue to explore and better understand Clear ice, the importance of addressing this topic in a comprehensive and thoughtful manner becomes evident. In this article, we will explore different perspectives and approaches on Clear ice, with the aim of deepening our understanding of this topic and its relevance in today's world.

For ice cubes, see Ice cube § Clear and cloudy.

Clear ice refers to a solid precipitation which forms when air temperature is between 0 °C (32 °F) and −3 °C (27 °F) and there are supercooled, relatively large drops of water (from freezing fog). A rapid accretion and a slow dissipation of latent heat of fusion favor the formation of a transparent ice coating, without air or other impurities. A similar phenomenon occurs when freezing rain or drizzle hits a surface and is called glaze. Clear ice, when formed on the ground, is often called black ice, and can be extremely hazardous.

Clear ice is denser and more homogeneous than hard rime; like rime, however, clear ice accumulates on branches and overhead lines, where it is particularly dangerous due to its relatively high density.

See also

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References

External links

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