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Structure and Properties of Lake Ice

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Book cover Freezing of Lakes and the Evolution of their Ice Cover

Abstract

In the Earth’s nature, water is the only substance, which occurs in all three phases: gas, liquid, and solid.

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Notes

  1. 1.

    Bismuth, gallium and germanium, for example, become less dense in the liquid–solid phase change. But the change is by far not so large than in water.

  2. 2.

    Frazil comes the French word fraisil, which refers to coal cinders.

  3. 3.

    Slush is water-saturated snow.

  4. 4.

    In glaciology where snow transforms into ice by compression, the density is taken as 830 kg m−3 at the transition (e.g., Paterson 1999), corresponding to the gas content of 9.5 %.

  5. 5.

    The thickness where irradiance has decreased to the fraction e−1, also called the e-folding thickness.

  6. 6.

    Inherent optical properties depend on the properties of the medium only, while apparent optical properties depend also on the directional distribution of the incoming light.

  7. 7.

    Sometimes the expression spectral albedo is used instead of surface reflectance.

  8. 8.

    Also know as yellow substance in optical oceanography.

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Correspondence to Matti Leppäranta .

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© 2015 Springer-Verlag Berlin Heidelberg

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Leppäranta, M. (2015). Structure and Properties of Lake Ice. In: Freezing of Lakes and the Evolution of their Ice Cover. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-642-29081-7_3

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