Search results
Results from the WOW.Com Content Network
The Spotter Network (SN) is a system that utilizes storm spotter and chaser reports of location and severe weather in a centralized framework for use by coordinators such as emergency managers, Skywarn and related spotter organizations, and the National Weather Service.
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 ...
In many areas, classes are conducted each spring in advance of the coming severe weather season. [2] Many SKYWARN spotters use methods to communicate with one another during severe storm events. A notable example of this is through the use of amateur radio nets , which is still an important method since severe weather can significantly disrupt ...
Thursday, March 14, 6:00pm - Skywarn Spotter Training - Rush County. Saturday, March 16, 9:00am - Skywarn Spotter Training - Owen County. Monday, March 18, 6:00pm - Skywarn Spotter Training - Vigo ...
Michigan fall colors: Week of Oct. 21. As we near the end of October, the predictor map expects that most of the state will have moved past peak color. The vibrant hues may still be present in ...
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.
Portions of southeast Michigan are under either a winter storm warning or winter weather advisory from 1 p.m. Friday to 7 p.m. Saturday.
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 ...