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Convective storm detection is the meteorological observation, and short-term prediction, of deep moist convection (DMC). DMC describes atmospheric conditions producing single or clusters of large vertical extension clouds ranging from cumulus congestus to cumulonimbus , the latter producing thunderstorms associated with lightning and thunder .
Convective available potential energy; Convective condensation level; Convective inhibition; Convective instability; Convective overshoot; Convective self-aggregation; Convective storm detection; Convective temperature; Cumulonimbus and aviation; Cumulonimbus cloud
In 1962 a research team from the United States Weather Bureau's National Severe Storms Project (NSSP) moved from Kansas City, Missouri to Norman, Oklahoma, where, in 1956, the Cornell Aeronautical Laboratory had installed a 3 cm continuous-wave Doppler Weather Surveillance Radar-1957 . This radar was designed to detect very high wind speeds in ...
Convective storm detection; Earth Observing System; Environmental monitoring; Geographic information system (GIS) Glossary of meteorology; Mesonet; Meteorology; Radiosonde; Rocketsonde; Surface weather observation; Timex Expedition WS4; Tropical cyclone observation; Weather reconnaissance; Weather radar; Weather satellite
A mesoscale convective complex (MCC) is a unique kind of mesoscale convective system which is defined by characteristics observed in infrared satellite imagery. Their area of cold cloud tops exceeds 100,000 square kilometres (39,000 sq mi) with temperature less than or equal to −32 °C (−26 °F); and an area of cloud top of 50,000 square ...
When people think of a thunderstorm, towering clouds on a warm and humid summer day may come to mind, but one thunderstorm tracked by forecasters over the Pacific Ocean several years ago set a ...
A mesoscale convective complex (MCC) is a unique kind of mesoscale convective system which is defined by characteristics observed in infrared satellite imagery. They are long-lived, often form nocturnally, and commonly contain heavy rainfall , wind , hail , lightning , and possibly tornadoes .
He was an organizer of and participant in the Bow Echo and Mesoscale Convective Vortex Experiment (BAMEX) of 2003 [2] and a researcher with the Pre-STORM Project of 1985. Przybylinski was a leading expert on quasi-linear convective systems (QLCS), bow echoes, and mesoscale convective systems (MCSs), and convective winds and tornadogenesis ...