Saturday,  June 23, 2012 • Vol. 12--No. 345 • 7 of 30 •  Other Editions

NWS Aberdeen WSR-88D to Receive Dual Polarization Upgrade

During a two-week period, beginning July 30, 2012, the Doppler radar at your National Weather Service Forecast Office will undergo an upgrade to incorporate new technology. For these two weeks, radar data will be unavailable from NWS Aberdeen! Surrounding radars include: Bismarck, ND, Grand Forks, ND, Duluth, MN, Minneapolis, MN, Sioux Falls, SD, North Platte, NE, and Rapid City, SD.
This much anticipated upgrade is part of the NWS vision to build a Weather-Ready Nation to better protect lives and livelihoods. This exciting upgrade will incorporate a new technology called dual-polarization, or dual-pol. This new technology will result in 14 new radar products that will enable us to continue providing our suite of high quality products and services to the public. This new technology and data will primarily help forecasters identify the type of precipitation that is falling as well as improve rainfall estimates

• Current NWS Doppler radars transmit and receive pulses of radio waves in a horizontal orientation. As a result, the radar only measures the horizontal dimensions of targets (e.g. cloud and precipitation droplets). Dual-polarimetric radar transmits and receives pulses in both a horizontal and vertical orientation. Therefore, the radar measures both the horizontal and vertical dimensions of targets. Since the radar receives energy from horizontal and vertical pulses, we can obtain better estimates of the size, shape, and variety of targets. It is expected that this will result in significant improvements in the estimation of precipitation rates, the ability to discriminate between precipitation types (e.g. hail vs. rain), and the identification of non-meteorological returns, such as chaff, ground clutter, and smoke plumes from wildfires that are not uncommonly detected by weather radar systems such as WSR-88D.

• Better estimation of total precipitation amounts
• Better estimation of the size distribution of hydrometeors (raindrops, snowflakes, hailstones, drizzle)

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