Snow flurry

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Snow flurry refers to a brief and light snowfall that results in little to no accumulation on the ground. Snow flurries are characterized by their short duration and light intensity, often occurring intermittently. They are a common weather phenomenon in regions that experience cold temperatures and are typically associated with winter weather patterns.

Characteristics

Snow flurries are typically light and sporadic, with snowflakes that are small and dry. Unlike snow showers, which can be more intense and lead to significant accumulation, snow flurries usually do not result in measurable snow on the ground. The visibility during snow flurries can be reduced, but it generally remains better than during heavier snow events.

Formation

Snow flurries form in a similar manner to other types of snowfall. They occur when cold air masses move over a region, causing the moisture in the air to condense and form snowflakes. These snowflakes then fall to the ground, but due to the light nature of the precipitation, they often do not accumulate significantly.

Impact

The impact of snow flurries is usually minimal compared to other forms of winter precipitation. They can create a picturesque scene and may cause minor visibility issues for drivers, but they rarely lead to hazardous conditions. However, in some cases, snow flurries can precede or follow more significant snow events, serving as an indicator of changing weather patterns.

Related Weather Phenomena

• Snow
• Snow shower
• Blizzard
• Sleet
• Freezing rain

See Also

• Winter storm
• Weather
• Meteorology
• Precipitation