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overshooting top वाक्य

"overshooting top" हिंदी मेंovershooting top in a sentence
उदाहरण वाक्यमोबाइल
  • Overshooting top of a cumulonimbus viewed from a plane crossing the Democratic Republic of Congo.
  • If the overshooting top is continuous it means the storm is probably a strong supercell.
  • This overshooting top will be noticeable by a colder temperature region in the thunderstorm on infrared images.
  • Whereas anvils form at the equilibrium level, overshooting tops continue to the maximum parcel level ( MPL ).
  • During a long-track tornado the whole top of the storm, including the overshooting top, might drop by thousands of feet.
  • Early on June 20, convection increased markedly with several overshooting tops ( denoted by cloud-top temperatures below ) appearing on satellite imagery.
  • An overshooting top lasting for more than 10 minutes is a sign of a strong updraft in a thunderstorm, indicating a strong likelihood that the storm is producing severe weather.
  • During a strong tornado, the overshooting top might roll over or fold over as new activity climbs up the back while the front of the overshooting top collapses into the storm.
  • During a strong tornado, the overshooting top might roll over or fold over as new activity climbs up the back while the front of the overshooting top collapses into the storm.
  • An empirical criterion for tornado formation has been developed by Dan Sowa from Northwest Orient Airlines as follows : the cumulonimbus overshooting top must enter into the stratosphere by at least 10000 feet.
  • Another signature associated with this situation is the Enhanced-V feature where the cold cloud tops forming at the overshooting top fan out in a V shape as cloud matter is blown downwind at that level.
  • An overshooting top forms when a thunderstorm's updraft, due to momentum from rapid ascent and strength of lifting, protrudes its equilibrium level, forming a dome-like structure on top of the anvil.
  • However, some exceptionally energetic convection processes-- notably volcanic overshooting tops associated with severe supercell thunderstorms-- may " locally " and " temporarily " inject convection through the tropopause and into the stratosphere.
  • Evidence of a supercell comes from the storm's shape and structure, and cloud tower features such as a hard and vigorous updraft tower, a persistent, large overshooting top, a hard anvil ( especially when backsheared against strong upper level winds ), and a corkscrew look or striations.
  • At various points of its evolution, it displayed textbook or record manifestations of supercell and derecho-related phenomena such as the right-mover supercell, evolution of supercells into a linear meso-scale feature which rapidly became a derecho, cumulonimbus with overshooting top and dome, bow echo, bookend vortices, regular and rotor downbursts, gust front, gustnado, rear inflow notch, classic derecho radar signature, effects of infrasound and atmospheric electricity, haboobs, and wind effects on bodies of water including seiches and exposure of bottoms of water features by the wind.

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