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Thundersnow, also known as a winter thunderstorm or a thundersnow storm, is a thunderstorm in which snow falls as the primary precipitation instead of rain. It is considered a rare phenomenon. [ 1 ] It typically falls in regions of strong upward motion within the cold sector of an extratropical cyclone .
The Watertown region received 8 to 12 in (20 to 30 cm) of snow with the cold front, but unfrozen Lake Ontario (in contrast to frozen Lake Erie), along with atmospheric conditions favorable for lake effect snow, allowed snow bands to form that resulted in storm totals of 66 in (168 cm) in Watertown, 72.5 in (184.2 cm) in Mansville, 93 in (236 cm ...
January 12–13, 1888. What made the storm so deadly was the timing (during work and school hours), the suddenness, and the brief spell of warmer weather that preceded it. In addition, the very strong wind fields behind the cold front and the powdery nature of the snow reduced visibilities on the open plains to zero.
Ball lightning is a possible source of legends that describe luminous balls, such as the mythological Anchimayen from Argentinean and Chilean Mapuche culture.. According to a statistical investigation carried out in 1960, of 1,962 Oak Ridge National Laboratory monthly role personnel, and of all 15,923 Union Carbide Nuclear Company personnel in Oak Ridge, found 5.6% and 3.1% respectively ...
A winter storm is an event in which wind coincides with varieties of precipitation that only occur at freezing temperatures, such as snow, mixed snow and rain, or freezing rain. In temperate continental and subarctic climates , these storms are not necessarily restricted to the winter season, but may occur in the late autumn and early spring as ...
This list of disaster films represents over half a century of films within the genre.Disaster films are motion pictures which depict an impending or ongoing disaster as a central plot feature.
Type 1: Stable and centered over burning area. Type 2: Stable or transient, downwind of burning area. Type 3: Steady or transient, centered over an open area adjacent to an asymmetric burning area with wind. There is evidence suggesting that the fire whirl in the Hifukusho-ato area, during the 1923 Great KantÅ earthquake, was of type 3. [15]
Alternatively, embers can be used to relight a fire after it has gone out without the need to rebuild the fire – in a conventional fireplace, a fire can easily be relit up to 12 hours after it goes out, provided that there is enough space for air to circulate between the embers and the introduced fuel.