Blue ice (glacial)
Blue ice occurs when snow falls on a glacier, is compressed, and becomes part of a glacier that winds its way toward a body of water. During its travels, air bubbles that are trapped in the ice are squeezed out, and the size of the ice crystals increases, making it blue. In some areas, earthquakes have raised the blue ice above the ground and created formations much like large frozen waves.
Small amounts of regular ice appear to be white because of plenty of air bubbles inside them and also because small quantities of water appear to be colourless. In glaciers, on the other hand, the pressure causes the air bubbles of the accumulated snow to be squeezed out increasing the density of the created ice. Large quantities of water appear to be blue, as it absorbs other colours more efficiently than blue, and therefore a large piece of compressed ice, or a glacier, would appear blue.
The blue color is sometimes wrongly attributed to Rayleigh scattering which is responsible for the color of sky. Rather, ice is blue for the same reason that large quantities of water are blue: it is a result of an overtone of an oxygen-hydrogen (O-H) bond stretch in water which absorbs light at the red end of the visible spectrum. In the case of oceans or lakes, some of the light, hitting the surface of water, is reflected back directly but most of it penetrates the suface interacting with its molecules. The water molecule can vibrate in different modes when light hits it. The red, orange, yellow, and green wavelengths of light are absorbed so that the remaining light we see is composed of the shorter wavelength blues and violets. This is the main reason why ocean color is blue. So, water owes its intrinsic blueness to selective absorption in the red part of its visible spectrum. The absorbed photons promote transitions to high overtone and combination states of the nuclear motions of the molecule, i.e. to highly excited vibrations.
Blue ice is exposed in areas of the Antarctic where there is no net addition or subtraction of snow. That is, any snow that falls in that area is counteracted by sublimation or other losses. These areas have been used as runways (e.g.Wilkins Runway, Novolazarevskaya, Patriot Hills Base Camp) due to their hard surface which is suitable for aircraft fitted with wheels rather than skis.
- Braun, Charles L.; Smirnov, Sergei N. (August 1993). "Why Is Water Blue?". J. Chem. Edu., 1993, 70(8), 612. Dartmouth College. Retrieved 2013-12-22.
- Harvey, Eveline (14 January 2011). "NZ blue ice sighting an unexpected treat for tourists". The New Zealand Herald. Retrieved 21 September 2011.
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