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It is observed that wind profiles during thunderstorms are affected by several factors with the major ones being distance from the thunderstorm cell centre, intensity of the storm and ground roughness.
Aircraft and radar measurements show that a single thunderstorm cell extends to an altitude of 8,000 to 10,000 metres (26,000 to 33,000 feet) and lasts about 30 minutes.
A haboob is a dust/sand/windstorm, usually caused by the collapse of a thunderstorm cell.
The sudden arrival of the thunderstorm cell amounted to "the perfect storm," Ward said.
A thunderstorm cell formed south of Long Island around 10 20 am, and became a supercell sometime later after interacting with a surface low-pressure center.
A severe thunderstorm cell in South Carolina produced five tornadoes that touched down, one of which killed a woman in her destroyed duplex while passing through Lexington County.
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The winds in the layer of the atmosphere that steers thunderstorm cells were blowing from west to east.
Finally, at singular points in these relations singularities are determined that mark qualitative shifts in the system, such as the formation of thunderstorm cells, the eye wall, and so on.
Stronger thunderstorm cells are capable of producing tornadoes and waterspouts.
Thunderstorm cells occasionally form in isolation, as the occurrence of one thunderstorm can develop an outflow boundary which sets up new thunderstorm development.
Thunderstorm cells occasionally form in isolation, as the occurrence of one thunderstorm can develop an outflow boundary that sets up new thunderstorm development.
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