![]() ![]() Since hail can cause the rainfall estimates to be higher than what is actually occurring, steps are taken to prevent these high dBZ values from being converted to rainfall. Hail is a good reflector of energy and will return very high dBZ values. Hartford, CT Doppler Radar Weather - Find local 06101 Hartford, Connecticut radar loop and radar weather images. ![]() Our interactive map allows you to see the local & national weather. These values are estimates of the rainfall per hour, updated each volume scan, with rainfall accumulated over time. See the latest Connecticut Doppler radar weather map including areas of rain, snow and ice. Depending on the type of weather occurring and the area of the U.S., forecasters use a set of rainrates which are associated to the dBZ values. The higher the dBZ, the stronger the rainrate. Typically, light rain is occurring when the dBZ value reaches 20. The scale of dBZ values is also related to the intensity of rainfall. The value of the dBZ depends upon the mode the radar is in at the time the image was created. Notice the color on each scale remains the same in both operational modes, only the values change. The other scale (near left) represents dBZ values when the radar is in precipitation mode (dBZ values from 5 to 75). One scale (far left) represents dBZ values when the radar is in clear air mode (dBZ values from -28 to +28). Each reflectivity image you see includes one of two color scales. The dBZ values increase as the strength of the signal returned to the radar increases. The closed-loop system response with the satisfactory tracking performance is shown. So, a more convenient number for calculations and comparison, a decibel (or logarithmic) scale (dBZ), is used. Radar Loop National Radar Map For Current Radar, See: NWS NOTE: We are diligently working to improve the view of local radar for Fairfield County - in the meantime, we can only show the US as a whole in static form. Reflectivity (designated by the letter Z) covers a wide range of signals (from very weak to very strong). TX and Silicon Valley Group Lithog- raphy Systems of Wilton, CT. "Reflectivity" is the amount of transmitted power returned to the radar receiver. the flying distances and loop - to - loop stunt of its prototype gliders. The colors are the different echo intensities (reflectivity) measured in dBZ (decibels of Z) during each elevation scan. ![]()
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