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Radar Application in Weather Forecast EECS 725 Chao Jiang 05/01/2015
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Radar Application in Weather Forecast Introduce to Weather Radar Typical Weather Radar Specification Limitation and Future Development
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Weather Radar Most of the weather radars are monostatic radars. Capable of detecting location of precipitation, calculating the motion of rain droplets, and its intensity. Usually operates in S-band and C-band. X-band weather radar is used only to detect nearby target, and Ka-band is used to research small-particle phenomenon. Ground, Airborne, and Spaceborne.
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Introduce to WSR-88D Weather Radar WSR-88D Network (160 Radars), operated by National Weather Service Deployed across the US in the 1990s. Was the first radar able to detect particle motions. Operates in S-band (Frequency: 3.1 GHz; wavelength: 10.5 cm)
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Basic Structure
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Dual-polarization
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Differentiating Rain and Snow. Detecting Hail Cores. Debris from Significant Tornadoes.
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Limitations (Beam Height) Due to the curvature of the Earth.
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Limitations (Beam Height)
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Limitations (Attenuation) Occurs when large objects scatter most of the microwave. Makes the storms behind the large object appear weaker
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Limitations (PRF constraints) PRF min = 2 Δf D PRF max = c/2R max Multiple scans at each angle Change PRF at the radar depending on the situation
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Future development (Phased Array) Consists of four stationary panels. Providing rapid scanning. Able to scan the sky in less than 1 minutes (more than 4 times faster than WSR-88D). Making the observation more accurate and reduce false alarms.
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Phased Array Radar in Norman, Oklahoma
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Reference http://www.meteor.iastate.edu http://www.wdtb.noaa.gov http://www.nssl.noaa.gov
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