Conclusion
•Cloud layer wind around 40 knots aided to transfer moisture/band 200-300km downwind of Lake Ontario
•Well established cutoff circulation from Sfc to 250mb led to limited shear and helped to transfer significant lake effect snow 200-300 km downwind of Lake Ontario
•Uni-directional flow between 250-260˚
•Cloud layer (0.5-3km) shear (CCL to Echo Top)≤ 30˚ Favorable for single well organized band (Niziol 1987)
•30˚ to 60˚ of shear multi band event/un-organized/less propagation downwind  (Produces less snowfall amounts and rates) (Niziol 1987)
1000-700mb lapse rates large depth to measure instability, deeper layer of instability.
1000-850mb shows strong lapse rates from sfc heating and very cold 85h temps (shows steep lapse rates many times throughout the winter