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  2. File:Water cycle.png - Wikipedia

    en.wikipedia.org/wiki/File:Water_cycle.png

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  3. File:Phase diagram of water.svg - Wikipedia

    en.wikipedia.org/.../File:Phase_diagram_of_water.svg

    English: Phase diagram of water as a log-lin chart with pressure from 1 Pa to 1 TPa and temperature from 0 K to 660 K, compiled from data in and . Note that the phases of Ice X and XI (hexagonal) differ from the diagram in .

  4. Ice spike - Wikipedia

    en.wikipedia.org/wiki/Ice_spike

    Water expands by 9% as it freezes. Occasionally the surface can freeze over except for a small hole; the continuing freezing and expansion of water that is below the surface ice then slowly pushes the remaining water up through the hole. Reaching very cold air, the edge of the extruded water freezes while remaining liquid in the center.

  5. Icicle - Wikipedia

    en.wikipedia.org/wiki/Icicle

    The wall of this ice tube is about 0.1 mm (0.004 in) and the width 5 mm (0.2 in). As a result of this growth process, the interior of a growing icicle is liquid water. The growth of an icicle both in length and in width can be calculated and is a complicated function of air temperature, wind speed, and the water flux into the icicle. [3]

  6. File:Ice-spice-logo.png - Wikipedia

    en.wikipedia.org/wiki/File:Ice-spice-logo.png

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  7. Mpemba effect - Wikipedia

    en.wikipedia.org/wiki/Mpemba_effect

    The phenomenon, when taken to mean "hot water freezes faster than cold", is difficult to reproduce or confirm because it is ill-defined. [4] Monwhea Jeng proposed a more precise wording: "There exists a set of initial parameters, and a pair of temperatures, such that given two bodies of water identical in these parameters, and differing only in initial uniform temperatures, the hot one will ...

  8. Ice pellets - Wikipedia

    en.wikipedia.org/wiki/Ice_pellets

    Ice pellets form when a layer of above-freezing air is located between 1,500 and 3,000 meters (5,000 and 10,000 ft) above the ground, with sub-freezing air both above and below it. This causes the partial or complete melting of any snowflakes falling through the warm layer (the French term for sleet, neige fondue , literally means "melted snow ...

  9. Clear ice - Wikipedia

    en.wikipedia.org/wiki/Clear_ice

    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 ...