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Published bySheena Armstrong Modified over 8 years ago
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Stephen Rodriguez, Jr. National Weather Service Chicago, IL
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Introduction Brief background. Purpose of Study. Synoptic background and forcing mechanisms. Synoptic/Mesoscale features: Moisture, Forcing, Instability. Conclusions.
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Radar Storm Evolution
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Observed Snowfall Totals CHICAGO
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Wind Gusts/Visbys/Lightning 1/4 MILE VISBYS. 65 STRIKES!
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Purpose of Study Synoptic/Mesoscale Overview. Pattern Recognition/Conceptual Models. “How to Forecast” Blizzards? What are we forecasting?
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Purpose - NWS Blizzard Definition Sustained wind or frequent gusts to 35 miles an hour or greater; and Considerable falling and/or blowing snow (i.e., reducing visibility frequently to less than ¼ mile). For a period of 3 hours or longer.
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Purpose - Blizzard Elements Heavy snowfall. Snow efficiency. Strong winds.
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Synoptic Overview 300 MB 02/02/11 00Z
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Synoptic Overview 700 MB 02/02/11 00Z
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Synoptic Overview 850 MB 02/02/11 00Z
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Synoptic Overview SFC 02/02/11 00Z
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Synoptic Overview 02/02/00 00Z ROAB KDVN
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00Z Low/Isallobaric Component 03Z06Z
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Well-Mixed Environment 04Z RUC Sounding
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Moisture 850 MB Moisture Transport
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Moisture TROWAL structure identifiable by 02Z-3Z. CHICAGO
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Forcing - Deformation
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Forcing - Isentropic Lift 22Z/00Z/02Z RUC 290K Persistent isentropic lift from late afternoon through late evening. CHICAGO
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Forcing - Frontogenesis RUC 02Z ORD MSN EVV
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Instability - EPV ORDEVVMSN RUC 02Z
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Instability – CAPE/Lapse Rates 04Z RUC Sounding NORTH CENTRAL ILLINOIS
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Snow Efficiency NORTH CENTRAL ILLINOIS 00Z-03Z
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Conclusions - Review Copious amounts of moisture. Persistent strong forcing due to both synoptic/meso forcing mechanisms. Instability – an added benefit. Snow efficiency.
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Conclusions – Key Factors Heavy Snowfall – Yes! Snow efficiency – Yes! Strong winds – Yes! Yes! Yes!!!
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Blizzard Climatology
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Conclusions – Lessons Learned Stick to “base” data. Pattern Recognition of three elements. All come together – Blizzard.
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Questions? References: NOAA/NWS/Storm Prediction Center Schwartz, 2001.
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