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supercooled water cloud
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In the 1930s, Bergeron and W. Findeisen developed the concept that clouds contain both supercooled water and ice crystals.
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This amount of water is further increased by the deposition of suspended and supercooled water droplets of the low clouds and, to the East of the watershed, by the enormous quantity of snow transported by the wind.
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As the hailstone ascends it passes into areas of the cloud where the concentration of humidity and supercooled water droplets varies.
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Such holes are formed when the water temperature in the clouds is below freezing, but the water, in a supercooled state, has not frozen yet due to the lack of ice nucleation.
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With highly unstable atmospheric conditions, large cumulus may continue to grow into cumulonimbus calvus (essentially a very tall congestus cloud that produces thunder), then ultimately into the species capillatus when supercooled water droplets at the top of the cloud turn into ice crystals giving it a cirriform appearance.
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By comparison, ice nucleation in supercooled water droplets is the controlling mechanism for the formation of high clouds in the upper troposphere.
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The droplets of liquid water in most tropospheric clouds above 2 or 3 km altitude are supercooled.
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High tropospheric and non-tropospheric clouds appear mostly white if composed entirely of ice crystals and/or supercooled water droplets.
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Below −20 °C (−4 °F), icing is rare because clouds at these temperatures usually consist of ice particles rather than supercooled water droplets.
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Within the month, Schaefer's colleague, the noted atmospheric scientist Dr. Bernard Vonnegut (brother of novelist Kurt Vonnegut) is credited with discovering another method for "seeding" supercooled cloud water.
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This process is temperature dependent, as supercooled water droplets only exist in a cloud that is below freezing.
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The cloud type associated with a thunderstorm, when the upper portion of the cloud exhibits glaciation (supercooled water droplets converting to ice crystals).
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Seeding of clouds requires that they contain supercooled liquid water—that is, liquid water colder than zero degrees Celsius.
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For cloud seeding to be successful, the clouds must contain sufficient supercooled water (water that has remained liquid at temperatures below the freezing point, 0°C/32°F).
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Hail forms in the cloud's main updraft winds in the form of supercooled water.
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A group of researchers from Europe and the United States arrived at this finding after examining supercooled water—which is found in most clouds and can transform into ice almost immediately—using two methods of X-ray analysis.
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Cloud seeding has been shown to be effective in altering cloud structure and size and in converting supercooled liquid water to ice particles.
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In an ideal model, a wave cloud consists of supercooled liquid water at the lower part, a mixed phase of frozen and liquid water near the ridge, and ice beginning slightly below the ridge and extending downstream.
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Such holes are formed when the water temperature in the clouds is below freezing but the water has not frozen yet due to the lack of ice nucleation (see supercooled water).
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19 sinne gevind in 9 ms. Hulle kom uit baie bronne en word nie nagegaan nie.