Thundersnow
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. It typically falls in regions of strong upward motion within the cold sector of an extratropical cyclone. Thermodynamically, it is not different from any other type of thunderstorm, but the top of the cumulonimbus cloud is usually quite low. In addition to snow, graupel or hail may fall as well. The heavy snowfall tends to muffle the sound of the thunder so that it sounds more like a low rumble than the loud, sharp bang that is heard during regular thunderstorms.
Thundersnow can occur during a normal snowstorm that sustains strong vertical mixing which allows for favorable conditions for lightning and thunder to occur. It can also occur from the lake effect or ocean effect thunderstorm which is produced by cold air passing over relatively warm water; this effect commonly produces snow squalls over the Great Lakes.
Occurrence
Americas
Within the United States, thundersnow is relatively rare but most common in "eastern Nevada and Utah, the central plains, and the Great Lakes states". Thundersnow also occurs in Nova Scotia and in the Northeastern United States, especially in New England and New York, sometimes several times per winter season. On December 30, 2019, a severe thunderstorm warning was issued for parts of Massachusetts for a thunderstorm cell that was producing "lightning, thundersnow, thundersleet, and thunderice". A "really rare" thundersnow storm occurred near Vancouver, British Columbia on December 17–18, 2022.The South Region of Brazil registered episodes of thundersnow in 1984 and 2005, in the state of Santa Catarina, and in August 2011, in some municipalities of the highland region of Serra Gaúcha, in the southern state of Rio Grande do Sul.
Europe
The British Isles and other parts of northwestern Europe occasionally report thunder and lightning during sleet or snow showers during winter and spring. Scotland registered an episode of thundersnow in the early hours of 4 December 2020, the unusual noise causing alarm among local people. The Met Office warned of thundersnow in Scotland, Wales and northern England in early January 2022.Western Europe has rare occurrences of thundersnow, as on 8 March 2010, when northeastern Catalonia, including Barcelona, experienced a heavy snowfall accompanied by lightning, with snow depths surpassing in low altitude areas.
In Central Europe, a large-area thundersnow occurred on 17 January 2022, when a strong synoptic-scale squall line passed north to south over whole central and eastern Poland, precipitating both granular snow and snowflakes, with discharge intensity exceeding 100 per minute. Other recent occurrences were in Poland and the Czech Republic in January 2023, Germany in January 2021, and Norway and Netherlands as well as Austria in April 2021, with previous occurrences in Norway in January 2019 and January 2020. Stockholm experienced thundersnow on 21 November 2022. It was detected once again in the Netherlands on 3 January 2026.
Asia
Low-pressure events in the eastern Mediterranean that originate from polar origin cause copious thundersnow occurrences during winter storms, especially over the elevated provinces of Israel, Jordan and Lebanon, including Amman and Jerusalem. When such storms happen at areas intended for skiing, the mountains are often evacuated for safety.Thundersnow is also common around Kanazawa and the Sea of Japan, and even around Mount Everest.
Formation
Thundersnow is caused by the same mechanisms as regular thunderstorms, but it is much more rare because cold dense air is less likely to rise.Lake effect precipitation
Lake effect thundersnow occurs after a cold front or shortwave aloft passes over a body of water. This steepens the thermal lapse rates between the lake temperature and the temperatures aloft. A difference in temperature of or more between the lake temperature and the temperature at about usually marks the onset of thundersnow, if surface temperatures are expected to be below freezing. However several factors, including other geographical elements, affect the development of thundersnow.The primary factor is convective depth. This is the vertical depth in the troposphere that a parcel of air will rise from the ground before it reaches the equilibrium level and stops rising. A minimum depth of is necessary, and an average depth of or more is generally accepted as sufficient. Wind shear is also a significant factor. Linear snow squall bands produce more thundersnow than clustered bands; thus a directional wind shear with a change of less than 12° between the ground and in height must be in place. However, any change in direction greater than 12° through that layer will tear the snow squall apart. A bare minimum fetch of is required so that the air passing over the lake or ocean water will become sufficiently saturated with moisture and will acquire thermal energy from the water.
The last component is the echo top or storm top temperature. This must be at least. It is generally accepted that at this temperature there is no longer any super cooled water vapour present in a cloud, but just ice crystals suspended in the air. This allows for the interaction of the ice cloud and graupel pellets within the storm to generate a charge, resulting in lightning and thunder.