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A storm spotter is a specific type of weather spotter. In the U.S., these volunteers are usually trained by the National Weather Service or local Skywarn group, and are given a phone number, internet outlet, or amateur radio frequency to report to if a severe weather event, such as a tornado, severe thunderstorm, or flash flood occurs where the ...
The US National Weather Service developed an organized storm spotter training system starting in the 1970's. Meteorologist Alan Moller played a significant role in the development of the effort. He believed that storm spotters are a vital part of the Integrated Warning System since they provide "ground truth verification" for forecasters.
Storm spotting – The observation of severe weather by individuals trained in weather and reporting. Spotters can be stationary or mobile. Storm Data (SD) – A National Climatic Data Center (NCDC) publication beginning in 1959 detailing quality controlled tornado and other severe weather summaries as the official NOAA record of such events.
The National Weather Service offers storm spotting training session to the public throughout Central Indiana. Indiana tornado season is approaching. Here's how to help spot severe weather
Storm chasing usually involves getting close enough to a tornado or severe storm to record its size and wind speed with the appropriate equipment. Many storm chasers have a background in meteorology.
Storm spotters are trained to discern whether a storm seen from a distance is a supercell. [8] They typically look to its rear, the main region of updraft and inflow. [8] Under the updraft is a rain-free base, and the next step of tornadogenesis is the formation of a rotating wall cloud. The vast majority of intense tornadoes occur with a wall ...
They are teaming up to host a free SKYWARN Storm Spotter class, presented by the National Weather Service, from 6 p.m. to 8 p.m. March 21 at the Southside Community Center, 2142 Alabama Highway 77.
Storm spotters are trained to discern whether or not a storm seen from a distance is a supercell. They typically look to its rear, the main region of updraft and inflow. Under that updraft is a rain-free base, and the next step of tornadogenesis is the formation of a rotating wall cloud. The vast majority of intense tornadoes occur with a wall ...