TRANSITION LINE This is known as the Correlation Coefficient on ST6 Radar. We use this in Winter Storms to see what is happening in the atmosphere with respect to particle sizes. The radar slices the atmosphere in the vertical and horizontal to find where particles change in size. The fuzzy look is the mix of snow and sleet. All snow to the north, all sleet to the south. Notice how it has hit a wall near I-78. It looks to stay here for the rest of the storm with snow piling up in the Poconos, an
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Example of using radar to diagnose what's hitting the ground. Left: Radar reflectivity Right: Correlation coefficient (CC) For CC, where it is dark red/near black, precip is uniform (same shape/size). Where it is green/blue, precip is not uniform (different shape/size). Where it is uniform (those reds/blacks) it is either all snow or all rain. (Snow here, rain further south - surface temps are a good proxy). Where there are those yellows/blues, that's a mix of rain/snow/sleet. | US National Weat
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Here is a radar animation from the time the tornado was reported in Harper County on Saturday. Displayed is storm relative velocity and correlation coefficient, showing the small tornado quickly tracking off to the north and northwest. | US National Weather Service Wichita Kansas
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Radar update 1:13 AM MDT: We use correlation coefficient to detect where precipitation is melting. Here this bright ring tells us that snow is melting to either sleet, rain or freezing rain. Depending on the temperature profile as the precipitation falls to the surface determines what the reported precipitation type will be. The height of this bright band tells us that from 3000 feet above the surface just outside of town. We should see change over to all snow in next couple hours. | US National
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