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Forecast Verification time!
Senor Perfect Forecast 74 81 5.5 ….
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DAY 2 DAY 2
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NAM precip during Tuesday (8 am – 8 pm)
E-Wall (Precip/ Temp/ Cloud)
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Weather Prediction Models
Dynamical / Physical Statistical Conceptual
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Computer Weather Model
Physical Models Equations ATTEMPT TO describe how atmosphere works Equations describe how atmosphere behaves (i.e. how it works)
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Statistical Weather Models
MOS
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(construct of the mind)
Conceptual Models (construct of the mind)
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Cyclogenesis – How storms form
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Surface Weather Map (radar overlay)
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L Sfc wx this morning H
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Penn State Weather Camps
Basic Weather Forecasting Guidelines Sat I – Sat II – Sat III - NWS – NHC - SPC - Radar - Radar - Radar sfc. map 1 - sfc. map EWALL - Soundings
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500 MB MODEL FORECAST (UPPER LEVELS)
This Afternoon L L H H
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THR 0z = ? 8 p.m. Wed NAM MODEL LIFTED INDEX LIFTED INDEX = measure of how unstable atmosphere is between sfc and 500mb
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...Pennsylvania into New York...
A belt of modest cyclonic flow aloft will reside over a moderately unstable warm sector ( J/kg MLCAPE). A few storms may develop along the cold front or lake breeze boundaries across the southern G. Lakes and spread southeast to PA. Mid-level lapse rates will be weak along with modest kt vertical shear. A few storms could produce locally strong wind gusts and marginal hail from afternoon to early evening. Soundings – vertical plots of T, w, q – great way to assess convective instability (at a single location)
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500 MB MODEL FORECAST (UPPER LEVELS)
This Afternoon Wind flow nearly parallel to isobars in upper levels = minimal friction
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Ms. Sally Climo 73 81 5 PA
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Penn State Weather Camps
Basic Weather Forecasting Guidelines Sat I – Sat II – Sat III - NWS – NHC - SPC - Radar - Radar - Radar sfc. map 1 - sfc. map EWALL - Soundings
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RH Calculator Relative Humidity – How close the air is to saturation
- Varies between? - If in a cloud ….. RH = ? Dew Point – Absolute humidity (how much H20 v) T = 85 D = 65 RH = 51% How can we make a cloud? RH Calculator
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