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In the cold winter months of regions East of the Rocky Mountains, a solid, dry, warm twist at times blows from the mountains over the land. These breezes, known as Chinook winds, can bring fast temperature changes.

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When the warm, dry, fast-moving Chinook winds pass over snow-covered areas, the snow often vaporizes before it has a chance to melt, according to the U.S. Geological Survey.

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An extraordinary case of a Chinook wind was recorded in South Dakota in January 1943, as per Black Hills Weather. The recorded temperature at 7:30 a.m. was less 4 F (less 20 C) and when the Chinook winds started soon after, the temperature expanded 49 degrees F (7 degrees C) in only two minutes and by 9 a.m., when the Chinooks subsided, occupants were encountering 54-degree (12 C) climate. At the point when the breezes faded away, it took 27 minutes for the temperature to drop 58 degrees, back to where it was in the first part of the day.

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What is a chinook? | Ask Our Meteorologist

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Corb Lund - Chinook Wind - Edmonton to Golden, BC Timelapse

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(Alex Sosnowski, 2018)

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Alex Sosnowski. A.S. (2018). AccuWeather. Retrived from: https://www.accuweather.com/en/weather-news/what-are-chinook-winds/70006865

U.S. Geological Survey. G.S. (2016). Sublimation and water cycle. Retrived from: https://www.usgs.gov/special-topic/water-science-school/science/sublimation-and-water-cycle?qt-science_center_objects=0#qt-science_center_objects