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The University of Oklahoma's RaXPol mobile Doppler weather radar, positioned at a nearby overpass, measured winds preliminarily analyzed as in excess of 296 mph (476 km/h). These winds are considered the second-highest ever measured worldwide, just shy of the 302 ± 22 mph (486 ± 35 km/h) recorded during the 1999 Bridge Creek–Moore tornado .
Despite the violence of the tornado and the presence of its associated mesocyclone aloft, the thunderstorm did not exhibit a distinct hook echo on weather radar typically associated with such tornadoes. This may have also been caused by the unusual southwestward motion of the thunderstorm, resulting in the tornado's placement in an atypical ...
Continuous-wave radar (CW radar) is a type of radar system where a known stable frequency continuous wave radio energy is transmitted and then received from any reflecting objects. Individual objects can be detected using the Doppler effect , which causes the received signal to have a different frequency from the transmitted signal, allowing it ...
Say you earn an income of $2,000 a month. Following the 50/30/20 rule would mean allocating $1,000 to needs, $600 to wants and $400 to savings or high-interest debt. But if your monthly rent and ...
To further put this all into perspective, only 63% of U.S. adults could cover a $400 emergency expense completely using “cash or its equivalent” (meaning that you pay using cash, savings or a ...
There’s only 10 out of 50 major metropolitan areas where a household earning the median income can put less than 20% down and still have an “affordable” payment on the typical home, Zillow ...
The Storm Prediction Center issues convective outlooks (AC), consisting of categorical and probabilistic forecasts describing the general threat of severe convective storms over the contiguous United States for the next six to 192 hours (Day 1 through Day 8). These outlooks are labeled and issued by day, and are issued up to five times per day.
As shown in the map to the left, there was up to 50 mm (2.0 in) of precipitable water in the warm air mass invading Southern Ontario with a strong southwesterly low level jet parallel to the cold front and the presence of an upper jet-stream. All of these were very favorable for the development of severe thunderstorms.
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