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Thundersnow

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Thundersnow

A rare winter thunderstorm where lightning crackles through falling snow/Weather & Climate

Thundersnow is a rare meteorological phenomenon in which thunder and lightning occur during a snowstorm. It happens when a layer of warm air near the surface rises rapidly through a colder layer above, creating the same convective instability that powers ordinary thunderstorms but in a winter setting. Lightning during thundersnow is typically closer to the ground and appears brighter because the snow-filled air reflects the flash. Thunder is often muffled by the snow, audible only within about 3 km instead of the usual 16 km. Thundersnow events frequently produce extremely heavy snowfall rates of 5 to 10 cm per hour and are most common around large lake-effect snow bands.

Measurements

Thunder audibility range3,000 m
15,000Plier lengths
42.4Boeing 747 lengths
Snowfall rate per hour7.5 hundredths m
2 hundredthsKayaks
1.03Lipstick tubes
1.12Tennis ball diameters

5 to 10 cm per hour

Typical lightning altitude500 m
16.7Church steeple heights
25Windmill heights
943Ukulele lengths
Surface temperature (typical)271 K
64.5Liquid helium baths
7.2 hundredthsWelding torches

About -2 C

Updraft speed15 m/s
5 millionthsPercent light speeds
750Typing fingers
4.3 tenthsCommuter trains
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