Tornado Shelf Cloud at Xavier Kirkby blog

Tornado Shelf Cloud. Most false tornado and false funnel cloud reports are associated with shelf clouds. They are larger and lack horizontal rotation which can form a tornado. A shelf cloud is a low, horizontal cloud formation typically associated with the leading edge of a gust front, which is the boundary between advancing cold air from a thunderstorm and warm air ahead. Remember, that the main threat with any squall line is severe damaging winds associated with the shelf cloud, although. As the shelf cloud passes, you can quickly feel the shift in wind direction and wind speeds pick up. You are feeling the gust front. As the warm, moist air condenses, you can see the shelf cloud. Shelf clouds are different because they are more vertical motion. Below is a brief review of what a shelf cloud, wall cloud, and funnel cloud look like. A wall cloud may also persistently rotate.

Amazing 'shelf cloud' captured as thunderstorms sweep through Kansas, USA Offbeat News Sky News
from news.sky.com

As the shelf cloud passes, you can quickly feel the shift in wind direction and wind speeds pick up. Shelf clouds are different because they are more vertical motion. You are feeling the gust front. A wall cloud may also persistently rotate. Remember, that the main threat with any squall line is severe damaging winds associated with the shelf cloud, although. As the warm, moist air condenses, you can see the shelf cloud. Most false tornado and false funnel cloud reports are associated with shelf clouds. They are larger and lack horizontal rotation which can form a tornado. A shelf cloud is a low, horizontal cloud formation typically associated with the leading edge of a gust front, which is the boundary between advancing cold air from a thunderstorm and warm air ahead. Below is a brief review of what a shelf cloud, wall cloud, and funnel cloud look like.

Amazing 'shelf cloud' captured as thunderstorms sweep through Kansas, USA Offbeat News Sky News

Tornado Shelf Cloud Remember, that the main threat with any squall line is severe damaging winds associated with the shelf cloud, although. Below is a brief review of what a shelf cloud, wall cloud, and funnel cloud look like. A shelf cloud is a low, horizontal cloud formation typically associated with the leading edge of a gust front, which is the boundary between advancing cold air from a thunderstorm and warm air ahead. Shelf clouds are different because they are more vertical motion. As the shelf cloud passes, you can quickly feel the shift in wind direction and wind speeds pick up. As the warm, moist air condenses, you can see the shelf cloud. A wall cloud may also persistently rotate. Most false tornado and false funnel cloud reports are associated with shelf clouds. Remember, that the main threat with any squall line is severe damaging winds associated with the shelf cloud, although. You are feeling the gust front. They are larger and lack horizontal rotation which can form a tornado.

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