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Deep Convection

Deep Convection. Ordinary Cells Multicell storms Supercells . Ordinary Cells. Cb – ordinary cells are the most basic form of convection Have been studied and documented since the late 1800’s:. Ordinary Cells.

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Deep Convection

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  1. Deep Convection Ordinary Cells Multicell storms Supercells

  2. Ordinary Cells Cb – ordinary cells are the most basic form of convection Have been studied and documented since the late 1800’s:

  3. Ordinary Cells The first well-known experiment on thunderstorms was “The Thunderstorm Project” in the mid 40’s Occurred over Florida in summer Collected surface, aircraft, sounding data Results of the experiment were published by Byers and Braham in 1949 in a book called “The Thunderstorm.” Check out: http://www.history.noaa.gov/stories_tales/thunder0.html

  4. Ordinary Cells Results from the Thunderstorm Project describe the evolution of an ordinary cell in three stages: 1) Cumulus Stage: developing Cu is dominated by updraft (< 10 m/s) Precip develops and is suspended by updraft

  5. Ordinary Cells 2) Mature Stage: Downdraft has now developed The downdraft is produced by precip loading and evaporative cooling Precip reaches the ground Leading edge of downdraft produces a gust front

  6. Ordinary Cells 3) Dissipating Stage: The cell is dominated by downdraft – is weak Light precip at the ground

  7. Ordinary Cells Life span is about 30-50 minutes Form in weakly sheared, convectively unstable environments Move at speed of mean environmental flow from 0-5,7 km Can produce rain, hail, high winds, rarely tornadoes

  8. Multi Cell Storms Can be thought of as a collection of ordinary cells in various phases of their life cycle: From Houze (93)

  9. Multi Cell Storms Note the air flow patterns, gust front, precip locations New storm development occurs on flank of gust front where convergence is maximized with low level storm relative ambient flow

  10. Multi Cell Storms New storm development occurs on flank of gust front where convergence is maximized with low level storm relative ambient flow Hence, cell motion (Vc) may be different than the system motion (Vs) Therefore, multicell storms may not propagate in the direction of the mean 0-5,7 km ambient flow

  11. Multi Cell Storms Cell motion versus system motion:

  12. Multi Cell Storms Form in larger sheared environments than ordinary cells The shear allows the updraft and downdraft to be separated Therefore, they can last for hours at a time Can produce copious rain, hail, high winds, some tornadoes on the gust front From Atkins et al. (04, mwr)

  13. Supercells Can be long-lived – 12 hrs at a time Have a single, quasi- steady rotating updraft Exhibit deviant motion from the mean flow, either to the left or right, mostly to the right Can produce, hail, high winds, significant tornadoes Can be very dangerous

  14. Supercells Early radar observations from Lemon and Doswell (79, mwr) Note: Forward flank downdraft and gust front Rear flank downdraft and gust front Up draft location Tornado location Hook Tornado location:

  15. FFD Supercells RFD Early radar observations from Lemon and Doswell (79, mwr) Note: FFD, updraft, and RFD updraft

  16. Supercells Early modeling results from Klemp and Rotunno (83, JAS) Note the similarities with the Lemon and Doswell observations

  17. Supercells Most always contain a bounded weak echo region (BWER)

  18. Supercells Most always contain a bounded weak echo region (BWER)

  19. Supercells Show deviant motion, both to the left and right of the mean flow They have also been observed to split:

  20. Supercells Modeled storms have also been observed to split:

  21. So, the following questions naturally arise: Given observations of the environment, which convective storm mode, or structure, should you anticipate? Ordinary cells Multi cells Supercells What environmental parameters should you look at? Instability Vertical wind shear What physical processes are responsible for the generation and evolution of the three aforementioned storm types?

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