1 / 40

Convective Systems: Squall lines and Bow Echoes

Convective Systems: Squall lines and Bow Echoes . ASP Colloquium 2006. Morris Weisman (NCAR/MMM). Radar Composite 7 May 1995 VORTEX. Radar Composite 26 May 1997. Radar Composite 11 June 2001. Squall Line Environments:. Bow Echoes: Fujita 1978. Bow Echoes: Fujita 1978.

lerato
Télécharger la présentation

Convective Systems: Squall lines and Bow Echoes

An Image/Link below is provided (as is) to download presentation Download Policy: Content on the Website is provided to you AS IS for your information and personal use and may not be sold / licensed / shared on other websites without getting consent from its author. Content is provided to you AS IS for your information and personal use only. Download presentation by click this link. While downloading, if for some reason you are not able to download a presentation, the publisher may have deleted the file from their server. During download, if you can't get a presentation, the file might be deleted by the publisher.

E N D

Presentation Transcript


  1. Convective Systems: Squall lines and Bow Echoes ASP Colloquium 2006 Morris Weisman (NCAR/MMM)

  2. Radar Composite 7 May 1995 VORTEX

  3. Radar Composite 26 May 1997

  4. Radar Composite 11 June 2001

  5. Squall Line Environments:

  6. Bow Echoes: Fujita 1978

  7. Bow Echoes: Fujita 1978

  8. 5 May 1996 18:48 GMT

  9. 5 May 1996 18:48 GMT

  10. 15 July 1995 Tree Blow Down in Adirondacks, 8 killed

  11. Symmetric, 2-D Squall Line

  12. Asymmetric Squall Line

  13. Houze et al. (BAMS, 1989)

  14. Houze et al. (BAMS, 1989)

  15. Surface Pressure Fields:

  16. So, how well do numerical models reproduce this observed spectrum?? Comet Web Modules: htpp://meted.ucar.edu/topics_convective.php • Convective Storm Matrix • MCS Matrix

  17. Symmetric, 2-D Squall Line

  18. RKW Theory Rotunno et al. (JAS, 1988) C/∆u > 1 “Optimal”condition for cold pool lifting C/∆u = 1 C/∆u < 1

  19. Early System Evolution “Optimal” C/∆u << 1 C/∆u ~ 1

  20. Mature System: C/∆u > 1

  21. Strength of Rear-Inflow Jet is proportional to CAPE

  22. 20 ms-1 shear, no Coriolis forcing

  23. How can we systematically produce the observed line-end vortex pattern?

  24. Line-end vortex mechanisms: Early Phase:

  25. Line-end vortex mechanisms: Mature Phase:

  26. Role of Line-End Vortices Focuses and Intensifies Rear-Inflow Jet

  27. Asymmetric Squall Line

  28. 20 ms-1 shear, Coriolis forcing

  29. Coriolis Effects:

  30. Symmetric-to-asymmetric evolution represents a generic property of finite-length squall lines in the presence of Coriolis forcing.

  31. IR Satellite from 27-28 May, 1998

  32. Radar Composite 28 May 1998

  33. X Upscale Growth of Convection Chris Davis (NCAR/MMM) Bow echoes 0540 UTC 10 June, 2003 MCV 0600 UTC 10 June, 2003 MCSs 11 June, 2003

More Related