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  1. The National Weather Service's 148 WSR-88D Doppler radars can detect most precipitation within approximately 90 mi of the radar, and intense rain or snow within...

  2. Jul 9, 2019 · Doppler radar works a little bit differently from older radars. Instead of merely just measuring the reflectivity of precipitation, it also detects the shape, position, and form as well. By measuring this, a Doppler radar can also measure the velocity of the movement of precipitation toward or away from the radar.

  3. Using and UnderstandingDoppler Weather Radar. Radar basics and the doppler shift. NEXRAD (Next Generation Radar) obtains weather information (precipitation and wind) based upon returned energy. The radar emits a burst of energy (green in the animated image). If the energy strikes an object (rain drop, snowflake, hail, bug, bird, etc), the ...

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  4. Sep 27, 2023 · All modern weather radars are Doppler radars. Therefore, the old-time radar sweeping line is no longer applicable. Some local television stations continue to show a sweeping radar on their broadcast; however the sweeping arm is computer-generated and just for show.

  5. Weather radar acts as a critical observational tool, detecting rain, snow, hail, damaging winds, and tornadic events while also aiding in forecasting weather patterns. The functionality of radar systems involves emitting electromagnetic waves and analyzing their reflection to determine the characteristics of precipitation.

  6. In the microwave portion of the electromagnetic spectrum, wavelengths vary between 1 millimeter and 1 meter. For Doppler radar, different wavelengths are used, including 10 centimeter (C-band), 5 centimeter (S-band), and 2 centimeter (X-band). The NEXRAD network’s 158 radars are predominantly C-band radars.

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  8. A Doppler radar is a specialized radar that uses the Doppler effect to produce velocity data about objects at a distance. [1] It does this by bouncing a microwave signal off a desired target and analyzing how the object's motion has altered the frequency of the returned signal.

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