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Supercooled water droplets or precipitation, used with types of present weather phenomena in accordance with Appendix 5.
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Supercooled water droplets or precipitation, used with types of present weather phenomena in accordance with Appendix 1.
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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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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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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 accretion rate of supercooled water droplets onto the hailstone depends on the relative velocities between these water droplets and the hailstone itself.
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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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Researchers conducted the first reported study of the freezing process of levitated single submicrometre-sized droplets in air using optical trapping techniques, including supercooled water droplets at 228 K.
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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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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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A hailstone grows larger when supercooled water droplets freeze on contact with a hailstone.
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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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Handful of graupel pellets. Under some atmospheric conditions, snow crystals may encounter supercooled water droplets.
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A handful of graupel pellets Falling graupel Under some atmospheric conditions, snow crystals may encounter supercooled water droplets.
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Falling graupel Under some atmospheric conditions, snow crystals may encounter supercooled water droplets.
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According to Bergeron, most precipitation is formed as a consequence of water evaporating from small supercooled droplets and accreting onto ice crystals, which then fall as snow, or melt and fall as cold rain depending on the ambient air temperature.
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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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Not all water freezes at 0 °C or 32 °F. Liquid water below this temperature is called supercooled, and such supercooled droplets cause the icing problems on aircraft.
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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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Graupel (also called soft hail or snow pellets)[1] refers to precipitation that forms when supercooled droplets of water are collected and freeze on a falling snowflake, forming a 2–5 mm (0.079–0.197 in) ball of rime.
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In clean and cold air, the micro-droplets of water that constitute a fog easily remain in this so-called "supercooling" state.
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22 sinne gevind in 13 ms. Hulle kom uit baie bronne en word nie nagegaan nie.