1 / 27

Shear Lines, Fronts and Areas of Confluence/Diffluence

Shear Lines, Fronts and Areas of Confluence/Diffluence. Mike Davison HPC International Desks. Shearlines vs. Fronts. Shear Lines: are associated with wind shifts (direction and speed).

Download Presentation

Shear Lines, Fronts and Areas of Confluence/Diffluence

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.


Presentation Transcript

  1. Shear Lines, FrontsandAreas of Confluence/Diffluence Mike Davison HPC International Desks

  2. Shearlines vs. Fronts • Shear Lines: are associated with wind shifts (direction and speed). • A line or narrow zone across which there is an abrupt change in the horizontal wind component parallel to this line • A line of maximum horizontal wind shear. • An area of directional wind confluence along the tail end of a surface front. • Lacks the baroclinicity/density discontinuity of surface fronts • Fronts: The interface or transition zone between two air masses of different density. • Density depends on temperature and moisture content • Fronts either lie along shear lines or can lag behind them.

  3. Wind Confluence and Diffluence in the Caribbean

  4. Wind Confluence and Diffluence in South America

  5. Wind Divergence

  6. Divergence of the Wind • We can express the divergence equation in a simplified form, with two terms: • Direction • Speed • The direction and speed terms, in-turn, can be expressed as directional/speed diffluence and confluence • Confluenceis not equal toConvergence • Diffluenceis not equal toDivergence

  7. Divergence (Cont) • Divergence/convergence calculations need to take into account the direction and speed terms. • This is done through objective analysis • Streamline analysis is a subjective technique, and it only shows directional diffluence and confluence. • It does not show convergence/divergence

  8. Example Directional Diffluence/Confluence Directional Confluence Directional Diffluence

  9. Speed Diffluence/Confluence Speed Confluence B A Speed Diffluence

  10. Convergent or Divergent? Directional Confluence A Speed Diffluence

  11. Convergent or Divergent?

  12. Convergent or Divergent? Speed Confluence A Directional Diffluence

  13. Convergent or Divergent?

  14. Evaluation of Shear Lines

  15. Front/Shear Line Evaluation

  16. Front and Shear Line

  17. Front and Shear Line

  18. Front and Shear Line

  19. Front and Shear Line

  20. Forecast Hints • During the Winter Months • Convective activity over the Gulf of Mexico and gulf coast of Mexico tends to be capped below 500 hPa (20,000 ft) • Evaluate upper dynamics for CONVERGENCE or DIVERGENCE before forecasting thunderstorms. • If models forecast post frontal northerlies of 25Kt or greater, and dew point temperature of 20C (68F) or greater over southern Mexico. • Forecast 12 hrs rainfall accumulation of at least 2-4 inches.

  21. Example of “Ideal” Conditions for Heavy Rainfall

  22. Example Front/Shear Line Caribbean

  23. Example Front/Shear Line South America

  24. Identify Features

  25. Satellite Interpretation

  26. Analysis

  27. Analysis

More Related