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Published byLogan Dalton Modified over 9 years ago
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Winter Weather Pattern Recognition
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Ice Storm (500mb) Trough or upper level low to the west o Source for upper level divergence (rising motion) and southerly winds which bring moisture and low-level warmer air northward Short wave trough or long wave trough generally to the northeast o Source of near surface cold air Cold front associated with the upper level trough Typically shallow arctic air
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Ice Storm (500mb)
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Ice Storm (850mb) Southerly component to the wind o Warm air advection Warm (above freezing) temperatures o Must melt the falling snow
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Ice Storm (850mb)
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Ice Storm (Surface) Surface temperatures obviously must be below freezing Low pressure to the west High pressure in the northern plains or upper Midwest Northerly component to the winds o Cold air advection
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Ice Storm (Surface)
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Typical Sounding
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Blizzard/Snow Storm (500mb) Long wave trough with embedded short wave trough or upper-level closed low o Upper-level low tends to track over northern Texas
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Blizzard/Snow Storm (500mb)
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Blizzard/Snow Storm (850mb) Low pressure to the east Cold air (below freezing) Northerly winds o Cold air advection o Frequently strong Blizzard Gulf moisture to the east or southeast o Advected around the cyclone
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Blizzard/Snow Storm (850mb)
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Blizzard/Snow Storm (Surface) Surface low to the east Sustained winds (or frequent gusts) of 35+ mph and visibility of less than ¼ mile o Must be present for at least 3 consecutive hours for a blizzard Dense packing of isobars (blizzard) o “Tight” pressure gradient Strong winds Northerly component to wind
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Blizzard/Snow Storm (Surface)
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Typical Sounding
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500mb Vorticity Average Tracks From Vanyo 2010
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Ice Storm, Blizzard, or Snow Storm? 1
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