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The WBNS TV Tower is a 839 ft (256 m) [1] tall free-standing lattice tower with a triangular cross section used by WBNS-TV in Columbus, Ohio. When originally completed in August 1948, the tower stood 595 ft (181 m) tall [ 2 ] making it one of the tallest freestanding towers in the United States at that time.
Rain gauges are used to measure the precipitation which falls at any point on the Earth's landmass. Remote sensing, as used in meteorology, is the concept of collecting data from remote weather events and subsequently producing weather information.
The exterior of a tipping bucket rain gauge The interior of a tipping bucket rain gauge. The tipping bucket rain gauge consists of a funnel that collects and channels the precipitation into a small seesaw-like container. After a pre-set amount of precipitation falls, the lever tips, dumping the collected water and sending an electrical signal.
Rain gauge for measuring liquid-equivalent precipitation; Ultrasonic snow depth sensor for measuring depth of snow; Pyranometer for measuring solar radiation; Unlike manual weather stations, automated airport weather stations cannot report the class and amount of clouds.
Weather radar in Norman, Oklahoma with rainshaft Weather (WF44) radar dish University of Oklahoma OU-PRIME C-band, polarimetric, weather radar during construction. Weather radar, also called weather surveillance radar (WSR) and Doppler weather radar, is a type of radar used to locate precipitation, calculate its motion, and estimate its type (rain, snow, hail etc.).
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The original precipitation accumulation measuring device used for automated airport weather stations was the heated tipping bucket rain gauge. The upper portion of this device consists of a 1-foot (0.30 m) diameter collector with an open top.
The term "Precipitation gauge" may refer to: Disdrometer, an instrument used to measure the drop size distribution and velocity of falling hydrometeors; Rain gauge, also known as an udometer, a pluviometer, an ombrometer or a cup is a type of instrument used by meteorologists and hydrologists to gather and measure the amount of liquid precipitation over a set period of time
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