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Low Pressure

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Low Pressure – PowerPoint PPT presentation

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Title: Low Pressure


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Low Pressure
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Today's Jet Stream
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Jet Stream - Zonal Flow
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Jet Stream - Meridonial Flow
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Pineapple Express
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Cold Front
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Warm Front
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Approaching Warm Front
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Stationary Front
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Stationary Front
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Occluded Front
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http//Billings Weather 040506
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Occluded Front
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Wall Clouds
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Tail Cloud
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Flanking Line
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The core of the updraft has the strongest
convective upward vertical velocity. This core of
rapidly rising air will only slow down and stop
when it encounters a very stable layer in the
atmosphere. This very stable layer is the
tropopause. Air will rise as long as it is less
dense and therefore more buoyant than surrounding
air. The faster air rises the longer it takes
generally to slow down and stop once it
encounters a very stable layer. This occurs
because a moving object has momentum. That part
of the updraft that has the greatest momentum
will form the overshooting top on a severe
thunderstorm. The diagram below shows the
overshooting top at "B".
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Overshooting Top
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