tsyl zaragoza maths fire jun 2009
DESCRIPTION
Simulación de IncendiosTRANSCRIPT
Operational Operational s imulation of fores t s imulation of fores t
firesfires
Santiago Monedero & Joaquín RamirezMaths & Fire Zaragoza 15/06/09Ingeniería del territorio http://www.tecnosylva.com
pp res entation outline res entation outline
2. Models
5. FFDSS GIS implementation
3. Rothermel implementation
4. Operational approach GIS
1. Introduction
Page 3
Us er´s need of operational tools Us er´s need of operational tools
•Many command centers has up to 30 fires a day in risk campaign
•Real need of quick fire dangerousness evaluation
•EVERY ALARM NEEDS A TECHNICAL EVALUATION OF DANGER
Galice, (SP) 2006
Page 4
Fire s imulation us e s ituation Fire s imulation us e s ituation
✂ Low use in European FF services of this kind of tools, unless in prevention phase, and in a few cases only (EUFIRELAB, 2005)1
Fires in euromediterranean countries are very fast, and a lot at the same time Actual tools are difficult to feed, and use data not fitted to the needs of the users Results needs of high skill users to get the best of them, and are difficult to evaluate
Use of propagator in PREVENTION and mainly USA – big fires
Bad perception of their utility, (lot of solutions, main approach of years of GIS developments in FF)
Input data hard to process and not appropiate scales
Results oriented more to laboratory than to real fire fighting
: Bas ic equations Local Radiation : Bas ic equations Local Radiation
RadiationDiffusion depends on temperature
Wind effects:Depends not only on wind but also on flame tilt
There is no explicitRadiation term
u: temperaturee: enthalpyy: fuel amountG(u): Multivalued operator for moisturef(u,y) reaction function (Arrenius type)
Vertical temperature loos
: Bas ic equations Local Radiation : Bas ic equations Local Radiation
Wind effects:Inside radiation term r
u: temperaturee: enthalpyy: fuel amountG(u): Multivalued operator for moisturer Explicit radiation
Multivalued operator
Moleding radiation and moisture content in fire spreadL. Ferragut, M. Asensio, S. Monedero Commun. Numer. Meth. Engng 2007; 23:819–833 Published online 19 October 2006 in Wiley InterScience (www.interscience.wiley.com). DOI: 10.1002/cnm.927
Radiation and moisture method presented in:
NumericalNumerical
•Mesh
•The resolution is done by the Finite Element Method with mesh adaptativity, we use the library Neptuno++ developed by Prof. Ferragut.
•Solution
•FEM example with 4 ignition points
Radiation models Radiation models
•Diffusion included: more complex
•Convection included in ff equation
•Diffusion included: slower
•Empirical model: hard to validate
•Not valid for complex surface
PROS CONS
LO
CA
LN
on L
OC
AL
•Valid for complex surfaces
•External independent model
•Validation independent of fire equations
•Wind effects only on radiation
: Empirical model exis ting s oftware : Empirical model exis ting s oftware
http://www.firemodels.org/
Rothermel
Potential fire risk analysis Table, graph, and diagram output
2-dimensional fire growth model
•ROS (Rate Of Spread)
•Fire line intensity
•Flame length
•Fuel type•Wind•Terrain•Moisture
f( )
Rothermel Implementation Rothermel Implementation
mdt
moisture
Fuel
V average
Rothermel(Behaveplus) ROS
Cost layer=time= L/ROS
Rate of Spread Implemented based on Rothermels, Albini paper
Time evolution Implemented based on an enhaced Esri’s Pathdistance function (Where the time variable is the accumulative cost)
With no extra hard work we obtain:graphs for homogeneus conditions like BehavePlusPotencial risk analysis like FlamMap
FireLAB FireLAB evolutionevolution : , FSPro FPA: , FSPro FPA
1 fire Several fires
1 meteo scenario
hundreds of meteo scenarios
FARSITE
FSPro FPA
FlamMap
Empirical model Empirical model
•Widely known used and tested
•Based on experimental data•NFFL fuel types •European fuel types
•Very quick resolution
•FREE!
•Surface fire, crown fire, spotting, Fire acceleration
•Very technical Only user with training may use it.
•Based experimental data•Bad exportability •No new effects are expected
•No FFDSS embeded GIS:•Data conversion•No operational layers•Tedious file configurations•No enhanced GIS capabilities
PROS CONS
High res olution fue l models High res olution fue l models
InfoGIS: SAD en Incendios Forestales
Fuel parameters OOA
USERS ASSESSMENT RESULTS: USERS ASSESSMENT RESULTS: Fuel ParametersFuel Parameters
Page 16
: Operational need High res o lution wind : Operational need High res o lution wind
• High Definition Wind Field: from Hirlam =13 km data to 25 m data
Fire lab Wind models Fire lab Wind models
Comparation of a Farsite simulation for low and high wind resolution (in white the actual perimeter of the fire).
Reference:The impact of high resolution wind field simulations on the accuracy of fire growth predictions (B. Butler, J. Forthofer, M. Finney)
Fire lab Wind models Fire lab Wind models
High Definition Wind High Definition Wind
Simulacion por FIRETEC. Referen ia: J. L. Winterkamp, R. R. Linn, Jonah J. Colman, William S. Smith
M.I Asensio, L. Ferragut, J. Simon, (2005). "A convective model for fire spread simulation."
Applied Mathematical Letters 18, pp. 673-677, 2005
Initial model presented on:
Enhaced with punctualWind value assimilation
’ : 2.5 Ferragut s Wind model’ : 2.5 Ferragut s Wind modelModelModel
•Should be valid for real time modeling•Takes into account: Vegetation friction and Temperature•Temperature dependent
•Fires own temperature (physical modeling of fire behaviour)•Sea breeze•Slope wind
•Punctual measurements•Fast calculations (400 x400 grid= 30 s.)¡
Bas ic local wind effec ts Bas ic local wind effec ts
Night.
ξ
Slope winds
+Temp
-Temp
Day.
+Temp
-Temp
-Day: 6 – 7 Km/h ¿?
-Night: 1 – 3 Km/h ¿?Temp (time, height (x,y))
SynergiesSynergies
spread Graphs Risk
RothermelPhysical FEM
Wind Spread
: FFDSS where tools s hould: FFDSS where tools s houldworkwork• InfoGIS is being used in operational way as the central
decission support system in the main spanish forest fires agencies since 1997– Castilla y León 1997 – Toledo 2000– Extremadura 2001– Aragón 2005– Andalucía 2006– Cantabria 2008
CENTRAL AUTONÓMICA
CENTRALESPROVINCIALES
CLIENTESLIGEROS
SERVICIOS ASOCIADOS (GPS, METEO)
SERVIDORCARTOGRAFÍA
WEB
19-20 October 2006, Page 24
Fire Platform Meeting
FFDSS
PROPAGATOR
INPUT DATA PROCESSOR
FIRE BEHAVIOUR
MODEL
OUTPUT DATA INTERFACE
InfoSIMInfoSIM s chemas chema
long lasting layerFuel, Satellite images, terrainShort lasting layersWind, moisture, etc
3D real timeOutput
Radiationmodel
FEMNeptuno++
G.I.S.
Physical fire model
•Help decision system•Satellite fire-front update•Satellite ignition detection
External
Moisturemodel
High DefinitionWind field
Model IModel II
Rothermel model
Rasterize
: InfoSIM operational fire propagator: InfoSIM operational fire propagator
• , , Original deve lopment PREVIEW projec t ins ide WFDSS
• Als o ArcGIS extens ion• One click s imulations
• Preras ter input data• Firebrak effec t• ( HR Wind Ferragut´s mode l• Management of s imulations• Integration with operational res ources
and fires data• 4 D res ults over HR imagery• Als o phys ical model
• : 2008 Tech Validation Extremadura& Andalus ian fires
• : 2009 Operacional us e campaign, , Extremadura UME Andalus ia & Aragón
(2010)
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Incendios registrados
( )Superficie total ha
< 1
1 - 5
5 - 10
10 - 50
> 50
## Conatos
:Integration of InfoSIM ins ide InfoGIS
InfoSIMInfoSIM
Res ults example
InfoSIMInfoSIM
Comparing with reality
InfoSIMInfoSIM
: 3 Operational res ults real time HR D : 3 Operational res ults real time HR DGISGIS
Propagadores de Incendios Forestales31
InputInputss - Outputs- Outputs
- Nationwide spatial database- HR fuel data – next steps: LIDAR ¡- HR firebreaks: BCN25- Formats
-Raster-Vector- Imagery (MODIS NDVI)
-Generic GIS, 3D OGC KML and FIRELAB (Farsite)-Generation of graphics, reports, (same as Farsite, Behaveplus & Flammap)
INPUTS
OUTPUTS
( )SIGYM METEOGRID
Integration of METEO GIS input data Integration of METEO GIS input data
Propagadores de Incendios Forestales33
motor de cálculo motor de cálculo
-Simulaciones Condiciones variables en el tiempo
Humedad vivo
Hora
Humedad Muerto
VientoModulo
Vientodirección
1 2 3
8 8 9
10 10 11
30 90 150
60
Propagadores de Incendios Forestales34
Firebraks trea Firebraks trea tmenttment
0 1 2 4 6 8 10 12 14 16 18 Anchura (metros)
0
R0
ROS = ROS0 * Parameter_firebreak
Null value: No effectHigh values : Low width, high effect
Propagadores de Incendios Forestales35
cc alculation engine alculation engine
-Adustment regional/ local factor (Farsite)
ROS = ROS * Parametro_fuel
- Fuel Model Inputs
Rothermel Albini
Custom
Burgan
Changes fuel behaviour,dep. experienceComb 1 12 0.33 0.64 0.811 1.7
Propagadores de Incendios Forestales36
cc alculation engine alculation engine
-3 different “pathdistance” temporal evolution
-Pathdistance standard8 y 16 directions
-Pathdistance 12 autoselecctable directions
Propagadores de Incendios Forestales37
Analis ys modules Analis ys modules
- Post-análisis (like Farsite)
Fuel surface / timePerimeter / time – for operation plansExpansion speed (Vx,Vy)Velocidad del “centro de masas” del incendioComparation with real perimeters
- Pre-análisis (like BehavePlus)
ROS, Flame length, intensitydepending on
Moisture1, moisture10, moisture100Moisture live, wind & slope
Propagadores de Incendios Forestales38
AutAut omated omated analianalis yss ys
- Capacity of extinction automated calculations
Configurable ROS, FL,Intensity – Eficiency (vs real data)
+ +
- Risk Indexes
ROSFLIntensity
December 16th-17th 2008, Page 39
Final Review - Toulouse
OperatiOperati : 3 onal us e UME Level : 3 onal us e UME LevelCPXCPX
TOA analisysCofrentes CPX UME Level 3 exercise (Valencia, Spain, april 2008)
Time for operational propagation tools ¡ Time for operational propagation tools ¡
Conclus ionsConclus ions
• Several models are available for real time fores t fire, modelling but lack of us e in operations
• FFDSS GIS bas ed s ys tems is the mandatory frame work to us e thes e models for practical us efulnes s
• Rothermel model is s till neces s ary for practical, us efulnes s us er´s confidence is increas ing
• A great s ynergy is generated by having all s ys tems:together
– , , , .FFDSS GIS Phys ical models Rothermel HR Wind
Thank you for y
our atte
ntion