Downscaling for Fire Weather – Forecasting in Complex Topography Heath Hockenberry National...

32
Downscaling for Fire Weather – Forecasting in Complex Topography Heath Hockenberry National Weather Service Fire Weather Program Manager

Transcript of Downscaling for Fire Weather – Forecasting in Complex Topography Heath Hockenberry National...

Page 1: Downscaling for Fire Weather – Forecasting in Complex Topography Heath Hockenberry National Weather Service Fire Weather Program Manager.

Downscaling for Fire Weather – Forecasting in Complex Topography

Heath HockenberryNational Weather Service Fire Weather Program Manager

Page 2: Downscaling for Fire Weather – Forecasting in Complex Topography Heath Hockenberry National Weather Service Fire Weather Program Manager.

Fire Weather – How are forecasts made?Fire Weather – How are forecasts made?

Like everything else, start with the broad model output.Like everything else, start with the broad model output.

Unlike everything else, apply basic conceptual Unlike everything else, apply basic conceptual knowledge of terrain and fuels.knowledge of terrain and fuels.

So how do we get from this….So how do we get from this…. To this ?To this ?

Page 3: Downscaling for Fire Weather – Forecasting in Complex Topography Heath Hockenberry National Weather Service Fire Weather Program Manager.

Fire Weather – “Old School” MeteorologyFire Weather – “Old School” Meteorology

Operational Fire weather is far from a complex, fine Operational Fire weather is far from a complex, fine scale model with fire feedbacks and parameterizations.scale model with fire feedbacks and parameterizations.Conceptual models are still the basis of forecasting in Conceptual models are still the basis of forecasting in complex terrain.complex terrain.

Essential readingEssential reading Essential TrainingEssential Training

Page 4: Downscaling for Fire Weather – Forecasting in Complex Topography Heath Hockenberry National Weather Service Fire Weather Program Manager.

S-190 Introduction to S-190 Introduction to Wildland Fire BehaviorWildland Fire Behavior

Basic Concepts and Terminology of Basic Concepts and Terminology of Wildland FireWildland Fire

Page 5: Downscaling for Fire Weather – Forecasting in Complex Topography Heath Hockenberry National Weather Service Fire Weather Program Manager.

Introduction to Fire Behavior TermsIntroduction to Fire Behavior TermsThis example…SpottingThis example…Spotting

Fire producing sparks or embers that are carried by Fire producing sparks or embers that are carried by the wind or convection that start new fires beyond the wind or convection that start new fires beyond the main firethe main fire

Page 6: Downscaling for Fire Weather – Forecasting in Complex Topography Heath Hockenberry National Weather Service Fire Weather Program Manager.

S-290 Introduction to S-290 Introduction to Wildland Fire BehaviorWildland Fire Behavior The “heart” of fire weather is taught in The “heart” of fire weather is taught in

this course…this course…StabilityStability WindsWinds

Page 7: Downscaling for Fire Weather – Forecasting in Complex Topography Heath Hockenberry National Weather Service Fire Weather Program Manager.

Adjustment to Temperature using Average Lapse Rate

S-290 TechniquesS-290 Techniques

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.

Page 8: Downscaling for Fire Weather – Forecasting in Complex Topography Heath Hockenberry National Weather Service Fire Weather Program Manager.

The thermal beltThe thermal belt Inversion DepthInversion Depth

S-290 TechniquesS-290 Techniques

Page 9: Downscaling for Fire Weather – Forecasting in Complex Topography Heath Hockenberry National Weather Service Fire Weather Program Manager.

S-390 and S-490 S-390 and S-490 Advanced Wildland Fire BehaviorAdvanced Wildland Fire Behavior

Wind Downscaling…Wind Downscaling…

• General Winds

• Local Winds

Page 10: Downscaling for Fire Weather – Forecasting in Complex Topography Heath Hockenberry National Weather Service Fire Weather Program Manager.

Examples of Local Wind circulations:

slope winds and sea breezes

Page 11: Downscaling for Fire Weather – Forecasting in Complex Topography Heath Hockenberry National Weather Service Fire Weather Program Manager.

20 FT WINDS RELATIONSHIP

20 ft winds = General Winds + Local Winds

Which dominates?General? Local? Both?

Page 12: Downscaling for Fire Weather – Forecasting in Complex Topography Heath Hockenberry National Weather Service Fire Weather Program Manager.

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 Due to the complexity of terrain and atmospheric interaction these are…atmospheric interaction these are…

DIFFICULT TO PREDICT!DIFFICULT TO PREDICT!

Page 13: Downscaling for Fire Weather – Forecasting in Complex Topography Heath Hockenberry National Weather Service Fire Weather Program Manager.

Terrain Correction Factors

Suggested General Wind correction factors:Suggested General Wind correction factors:

Assuming:Assuming: Gently sloped terrain.Gently sloped terrain. Neutral or unstable (or above inversion).Neutral or unstable (or above inversion). Windward slope exposed to general winds.Windward slope exposed to general winds.

Upper 1/3 of slope: 0.4 to 0.6 of General WindUpper 1/3 of slope: 0.4 to 0.6 of General Wind

Middle 1/3 of slope: 0.3 to 0.4 of General WindMiddle 1/3 of slope: 0.3 to 0.4 of General Wind

Lower 1/3 of slope: 0.2 to 0.3 of General WindLower 1/3 of slope: 0.2 to 0.3 of General Wind

Sheltered Areas: near zeroSheltered Areas: near zero

Page 14: Downscaling for Fire Weather – Forecasting in Complex Topography Heath Hockenberry National Weather Service Fire Weather Program Manager.

Terrain Correction Factors Example

0-1 mph6 mph

6 mph6 mph

Local slope windsLocal slope winds

Page 15: Downscaling for Fire Weather – Forecasting in Complex Topography Heath Hockenberry National Weather Service Fire Weather Program Manager.

Terrain Correction Factors Example

0-1 mph5 mph

7 mph10 mph

General WindsGeneral Winds

20 mph

Page 16: Downscaling for Fire Weather – Forecasting in Complex Topography Heath Hockenberry National Weather Service Fire Weather Program Manager.

Terrain Correction Factors Example

2 mph11 mph

13 mph16 mph

20 ft Winds=20 ft Winds=General Winds + Local WindsGeneral Winds + Local Winds

20 mph

Page 17: Downscaling for Fire Weather – Forecasting in Complex Topography Heath Hockenberry National Weather Service Fire Weather Program Manager.

Terrain Correction Factors Example

20 ft Winds=20 ft Winds=General Winds + Local WindsGeneral Winds + Local Winds

0 mph2 mph

2 mph16 mph

20 mph

Page 18: Downscaling for Fire Weather – Forecasting in Complex Topography Heath Hockenberry National Weather Service Fire Weather Program Manager.

High Elevation Gaps

Strong pass winds can also result from upperwinds combined with a low level pressure gradient.

Page 19: Downscaling for Fire Weather – Forecasting in Complex Topography Heath Hockenberry National Weather Service Fire Weather Program Manager.

Advanced Incident Advanced Incident Meteorology ForecastingMeteorology ForecastingForecasting on an Incident Management Team…Forecasting on an Incident Management Team…

Page 20: Downscaling for Fire Weather – Forecasting in Complex Topography Heath Hockenberry National Weather Service Fire Weather Program Manager.

Satellite Dish allows ingest and dissemination of forecast products

Page 21: Downscaling for Fire Weather – Forecasting in Complex Topography Heath Hockenberry National Weather Service Fire Weather Program Manager.

IMET ForecastingIMET Forecasting

Why Pibals?Why Pibals?Diurnal Wind Patterns.Diurnal Wind Patterns.Complex Terrain.Complex Terrain.Smoke/Public Health ConcernsSmoke/Public Health ConcernsModel problems!!!!Model problems!!!!

Page 22: Downscaling for Fire Weather – Forecasting in Complex Topography Heath Hockenberry National Weather Service Fire Weather Program Manager.

July 7th 2003 Brent Wachter

Incident Management Team Worried about the forecasted Gap wind Event

East Flank of Fire Left Alone →

↑ East

South →

↓ West

Page 23: Downscaling for Fire Weather – Forecasting in Complex Topography Heath Hockenberry National Weather Service Fire Weather Program Manager.

← Air Tanker Drop

Protect Taos Pueblo and Taos to the West

Page 24: Downscaling for Fire Weather – Forecasting in Complex Topography Heath Hockenberry National Weather Service Fire Weather Program Manager.

IMET ForecastingIMET Forecasting

Page 25: Downscaling for Fire Weather – Forecasting in Complex Topography Heath Hockenberry National Weather Service Fire Weather Program Manager.

Sanford FireSanford Fire

Data: Rick Stratton, SEM, Missoula Fire Lab

Page 26: Downscaling for Fire Weather – Forecasting in Complex Topography Heath Hockenberry National Weather Service Fire Weather Program Manager.

Sanford Fire Fuel

Page 27: Downscaling for Fire Weather – Forecasting in Complex Topography Heath Hockenberry National Weather Service Fire Weather Program Manager.

ENGLISH8 12 0 600 1700 54 87 50 20 75008 13 0 600 1700 52 88 50 20 75008 14 0 600 1700 52 88 50 25 75008 15 0 600 1700 57 87 50 27 75008 16 0 600 1700 56 81 50 23 75008 17 0 600 1700 57 81 50 20 75008 18 0 600 1700 53 81 50 21 7500

WTR Weather Stream File for FARSITE

Page 28: Downscaling for Fire Weather – Forecasting in Complex Topography Heath Hockenberry National Weather Service Fire Weather Program Manager.
Page 29: Downscaling for Fire Weather – Forecasting in Complex Topography Heath Hockenberry National Weather Service Fire Weather Program Manager.

IMET ForecastingIMET Forecasting

Page 30: Downscaling for Fire Weather – Forecasting in Complex Topography Heath Hockenberry National Weather Service Fire Weather Program Manager.

Regression Equations TechniquesRegression Equations TechniquesNational Fire Danger Rating National Fire Danger Rating Forecasts from local NWS Forecasts from local NWS Offices.Offices.

Multiple Regression for Grassy Mtn RAWS - Summer Min Eq

y=(.34A)+(0.037B)+(-0.0021C)+(0.62D)+2.3 R2=0.86

0

20

40

60

80

0 20 40 60 80

Boise Min Temp

Gra

ss

y M

in T

em

p

Grassy fcst

Fire-business driven fuel Fire-business driven fuel dryness prediction, tailoring dryness prediction, tailoring broad scale models to predict broad scale models to predict fuels’ receptiveness to fire.fuels’ receptiveness to fire.

Page 31: Downscaling for Fire Weather – Forecasting in Complex Topography Heath Hockenberry National Weather Service Fire Weather Program Manager.

DGEX vs. GFS DGEX vs. GFS (Model Downscaling)(Model Downscaling)http://wwwt.emc.ncep.noaa.gov/mmb/mmbpll/dgexhome.ops/http://wwwt.emc.ncep.noaa.gov/mmb/mmbpll/dgexhome.ops/

500 mbht/Vort

850 mbwind

Page 32: Downscaling for Fire Weather – Forecasting in Complex Topography Heath Hockenberry National Weather Service Fire Weather Program Manager.

AcknowledgementsAcknowledgements

NWS Mets and IMETs Chuck Redman, Coleen NWS Mets and IMETs Chuck Redman, Coleen Decker, Chris Gibson, Brent Wachter, Jim Decker, Chris Gibson, Brent Wachter, Jim Prange, Bob Servick, Julia Rutherford, Bernard Prange, Bob Servick, Julia Rutherford, Bernard Meier, Larry VanBussum, and Chuck Baker.Meier, Larry VanBussum, and Chuck Baker.

Predictive Services GACC Mets Terry Marsha, Predictive Services GACC Mets Terry Marsha, John Saltenberger and Tim Mathewson.John Saltenberger and Tim Mathewson.

NCEP’s Geoff DiMego.NCEP’s Geoff DiMego.

The National Interagency Fire Center Training The National Interagency Fire Center Training Branch.Branch.