1 / 32

Downscaling for Fire Weather – Forecasting in Complex Topography

Downscaling for Fire Weather – Forecasting in Complex Topography. Heath Hockenberry National Weather Service Fire Weather Program Manager. Fire Weather – How are forecasts made?. Like everything else, start with the broad model output.

laszlo
Download Presentation

Downscaling for Fire Weather – Forecasting in Complex Topography

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. Downscaling for Fire Weather – Forecasting in Complex Topography Heath HockenberryNational Weather Service Fire Weather Program Manager

  2. Fire Weather – How are forecasts made? • Like everything else, start with the broad model output. • Unlike everything else, apply basic conceptual knowledge of terrain and fuels. So how do we get from this…. To this ?

  3. Fire Weather – “Old School” Meteorology • Operational Fire weather is far from a complex, fine scale model with fire feedbacks and parameterizations. • Conceptual models are still the basis of forecasting in complex terrain. Essential reading Essential Training

  4. S-190 Introduction to Wildland Fire Behavior Basic Concepts and Terminology of Wildland Fire

  5. Introduction to Fire Behavior TermsThis example…Spotting • Fire producing sparks or embers that are carried by the wind or convection that start new fires beyond the main fire

  6. S-290 Introduction to Wildland Fire Behavior Stability Winds The “heart” of fire weather is taught in this course…

  7. S-290 Techniques Adjustment to Temperature using Average Lapse Rate Known: Elevations and the temperature at the lowest elevation Elevation Change: 2000 feet Average Lapse Rate -3.5F/1000 feet Simple calculations like this are done all the time in fire weather, for temperature adjustments.

  8. S-290 Techniques The thermal belt Inversion Depth

  9. Wind Downscaling… S-390 and S-490 Advanced Wildland Fire Behavior • General Winds • Local Winds

  10. Examples of Local Wind circulations:slope winds and sea breezes

  11. 20 FT WINDS RELATIONSHIP 20 ft winds = General Winds + Local WindsWhich dominates?General? Local? Both?

  12. Terrain Forced Flows The effects of terrain on General Winds: • Dissipation of wind by terrain features • Acceleration of wind by terrain features • Diversion of wind around terrain features Due to the complexity of terrain and atmospheric interaction these are… DIFFICULT TO PREDICT!

  13. Terrain Correction Factors Suggested General Wind correction factors: • Assuming: • Gently sloped terrain. • Neutral or unstable (or above inversion). • Windward slope exposed to general winds. Upper 1/3 of slope: 0.4 to 0.6 of General Wind Middle 1/3 of slope: 0.3 to 0.4 of General Wind Lower 1/3 of slope: 0.2 to 0.3 of General Wind Sheltered Areas: near zero

  14. Terrain Correction Factors Example 6 mph 6 mph 6 mph 0-1 mph Local slope winds

  15. Terrain Correction Factors Example 20 mph 10 mph 7 mph 5 mph 0-1 mph General Winds

  16. Terrain Correction Factors Example 20 mph 16 mph 13 mph 11 mph 2 mph 20 ft Winds=General Winds + Local Winds

  17. Terrain Correction Factors Example 20 mph 16 mph 2 mph 2 mph 0 mph 20 ft Winds=General Winds + Local Winds

  18. High Elevation Gaps Strong pass winds can also result from upper winds combined with a low level pressure gradient.

  19. Forecasting on an Incident Management Team… Advanced Incident Meteorology Forecasting

  20. Satellite Dish allows ingest and dissemination of forecast products

  21. IMET Forecasting • Why Pibals? • Diurnal Wind Patterns. • Complex Terrain. • Smoke/Public Health Concerns • Model problems!!!!

  22. Incident Management Team Worried about the forecasted Gap wind Event ↑ East East Flank of Fire Left Alone → South → ↓ West July 7th 2003 Brent Wachter

  23. Protect Taos Pueblo and Taos to the West ← Air Tanker Drop

  24. IMET Forecasting

  25. Sanford Fire Data: Rick Stratton, SEM, Missoula Fire Lab

  26. Sanford Fire Fuel

  27. WTR Weather Stream File for FARSITE ENGLISH 8 12 0 600 1700 54 87 50 20 7500 8 13 0 600 1700 52 88 50 20 7500 8 14 0 600 1700 52 88 50 25 7500 8 15 0 600 1700 57 87 50 27 7500 8 16 0 600 1700 56 81 50 23 7500 8 17 0 600 1700 57 81 50 20 7500 8 18 0 600 1700 53 81 50 21 7500

  28. IMET Forecasting

  29. Regression Equations Techniques • National Fire Danger Rating Forecasts from local NWS Offices. • Fire-business driven fuel dryness prediction, tailoring broad scale models to predict fuels’ receptiveness to fire.

  30. DGEX vs. GFS (Model Downscaling)http://wwwt.emc.ncep.noaa.gov/mmb/mmbpll/dgexhome.ops/ 500 mb ht/Vort 850 mb wind

  31. Acknowledgements • NWS Mets and IMETs Chuck Redman, Coleen Decker, Chris Gibson, Brent Wachter, Jim Prange, Bob Servick, Julia Rutherford, Bernard Meier, Larry VanBussum, and Chuck Baker. • Predictive Services GACC Mets Terry Marsha, John Saltenberger and Tim Mathewson. • NCEP’s Geoff DiMego. • The National Interagency Fire Center Training Branch.

More Related