USING MID-LEVEL THICKNESS PATTERNS AND WARM AIR ADVECTION TO FORECAST HEAVY SNOW
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Forecasting heavy snow has always been a challenge to forecasters. They have to rely cm a variety of techniques to make quality forecasts. Mary of these techniques require choosing a path for the surface low and/or 500 mb vorticity maximum. In the age of multiple numerical models, determining the actual path of a feature, such as a 500 mb vorticity iraximum, becomes difficult because the models often provide divergent solutions. Mary times, reasons to select one model over another are hard to justify. 1988 NWS (National Weather Service) NWC (National Water Center) Library Public Domain 1931
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NOAA
创建时间：
2021-10-05
