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Fire Ecology Pete Fulé Northern Arizona University.
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Transcript of Fire Ecology Pete Fulé Northern Arizona University.
Fire Ecology
Pete FuléNorthern Arizona University
1)Fire regimes
2)Fire history methods
a) Fire scarsb) Comparison to records
3)Fire and climate
4)Effects of forest restoration on fire behavior
5)Future fires: drought & beetles
Overview
Frequency
High frequency Low frequencyIntensity High intensity High intensity
(e.g., FL Everglades) (e.g., boreal, subalpine, lodgepole)
High frequency Low frequencyLow intensity Low intensity(e.g., ponderosa pine) (some deserts?)
Fire Regimes
Fire History Methods
Fire scars — common technique in surface-fire ecosystems.
Advantages: exact dates (even seasons of fires), locations of scarred trees.
Disadvantages: can’t map fire perimeter, absence of scars ≠ absence of fire.
Stand age — common technique in stand-replacing ecosystems.
Advantages: map perimeter/area of fire.
Disadvantages: imprecise fire date, newer fires obliterate evidence of older ones.
How good are fire scar methods? Critiqued by Baker & Ehle (2001, Can. J. Forest Research 31:1205-1226)
Comparison to Fire Records
• Across western North America, we usually find sites with good records but no fires (USA), or many fires but limited records (Mexico).
Comparison to Fire Records
• Across western North America, we usually find sites with good records but no fires (USA), or many fires but limited records (Mexico).
• Grand Canyon has both: earliest recorded fire is the 1924 “Powell” fire.
Comparison to Fire Records
• Across western North America, we usually find sites with good records but no fires (USA), or many fires but limited records (Mexico).
• Grand Canyon has both: earliest recorded fire is the 1924 “Powell” fire.
• Independent fire scar analysis found each of the 13 recorded fires > 20 acres since 1924 on the Powell, Rainbow, & Fire Pt. study sites (total of 1700 acres).
Fulé, P.Z., T.A. Heinlein, W.W. Covington, and M.M. Moore. 2003. Assessing fire regimes on Grand Canyon landscapes with fire scar and fire record data. International Journal of Wildland Fire 12(2):129-145.
August 10-24, 1993
Final size: 138 ha
Stars indicate six samples thatrecorded the fire
Six additional samples did notrecord the fire
Emerald Prescribed Natural Fire
Fire History 1700 to 1997All Fires
Fires scarring 25%or more of the samples
Fire History 1700 to 1997All Fires
Fires scarring 25%or more of the samples
Fulé, P.Z., T.A. Heinlein, W.W. Covington, and M.M. Moore. 2000. Continuing fire regimes in remote forests of Grand Canyon National Park. USDA Forest Service Proceedings RMRS-P-15-VOL-5: 242-248.
Powell Plateau, Grand Canyon National Park
Mixed Conifer
Mid elevation site (2500 m):
Swamp RidgeNorthwest III
Fire frequency:6-9 years
Last fire 1879
Forest: mixed conifer, formerly ponderosa pine
Swamp Ridge, Grand Canyon N.P.
High elevation sites (2550-2800 m):
Little Park
Fire frequency:complex patterns, MFI25%= 31 yrMFIPoint= 32 yrWt avg of fire-initiated stands = 22 yrs
Last fire 1879
Forest: aspen, mixed conifer, spruce-fir
Current Forest
Structure(circa 2000)
Simulate 1880-2040
1880 Forest Structure
CrownBiomass
CrowningIndex
FVS
Dendro
Intersecting evidence:• Lang & Stewart survey (1910)• Historical photos & data• Rasmussen (1941)
Compared to measured data in 2000, +/- 20%
Tested procedures
Forest Simulation and Fire Behavior Modeling
Add regen
Compared to observed fire behavior (NWIII fire & Outlet fire)
Landscape Maps 1880-2040
Forest Plan
Fire PlanSmoke
Wildlife Biomass equations
Nexus
Fire weather
Site data
Crown biomass changes in Grand Canyon forests, 1880-2040
Crown Biomass Changes 1880-2040
0
6000
12000
18000
1880 1900 1920 1940 1960 1980 2000 2020 2040
Decade
Cro
wn
Bio
mas
s (k
g/ha)
FP
RP
PP
SR
BS
LP
Percent Mesic Species
1880:
30% @ 2500 m65% @ 2650 m86% @ 2700 m
2040:
60% @ 2500 m86% @ 2650 m96% @ 2700 m
Fulé, P.Z., J.E. Crouse, A.E. Cocke, M.M. Moore, and W.W. Covington. 2003. Changes in canopy fuels and potential fire behavior 1880-2040: Grand Canyon, Arizona. Final Report to the Joint Fire Science Program, CA-1200-99-009-NAU 04 (Part 2).
Kaibab National Forest
Grand Canyon National Park
Site Elev. Veg. MFI*
1) Powell Plateau
2296 Pine 4.5
2) Fire Point 2338 Pine 4.9
3) Rainbow Plateau
2320 Pine 5.3
4) Galahad Point
2350 Pine 4.0
5) Swamp Ridge
2482 Mix Con 7.1
6) Big Spring 2650 Aspen,Spruce
31
7) Little Park 2724 Aspen,Spruce
31
12
3
4
5 6 7
* Mean Fire Interval (10%-scarred < 2,500 m)
Fulé, P.Z., T.A. Heinlein, W.W. Covington, and M.M. Moore. 2003. Assessing fire regimes on Grand Canyon landscapes with fire scar and fire record data. International Journal of Wildland Fire 12(2).
Fulé, P.Z., J.E. Crouse, T.A. Heinlein, M.M. Moore, W.W. Covington, and G. Verkamp. 2003. Mixed-Severity Fire Regime in a High-Elevation Forest: Grand Canyon, Arizona. Landscape Ecology 18:465-486.
Kaibab Plateau, Arizona
Fire and Climate
• Climate is the major factor influencing distribution of ecosystems and occurrence of “fire weather”.
• Southwest has frequent fires because climate is dry, hot, and windy nearly every summer.
• Climate causes synchrony in burning across landscapes, mountain ranges, states.
• Drought affects likelihood of fire.
• El Niño/Southern Oscillation affects likelihood of fire.
Swetnam, T.W., and C.H. Baisan. 2003. Tree-ring reconstructions of fire and climate history in the Sierra Nevada and southwestern United States. In: T.T. Veblen, W.L. Baker, G. Montenegro, and T.W. Swetnam (Editors), Fire and Climatic Change in Temperate Ecosystems of the Western Americas, Springer, New York, pp. 158-195.
Synchrony of Major Fire Years in the Southwest
Fire-ENSO Relationship Across the Southwest
Swetnam, T.W., and C.H. Baisan. 2003. Tree-ring reconstructions of fire and climate history in the Sierra Nevada and southwestern United States. In: T.T. Veblen, W.L. Baker, G. Montenegro, and T.W. Swetnam (Editors), Fire and Climatic Change in Temperate Ecosystems of the Western Americas, Springer, New York, pp. 158-195.
Pumpkin Fire (2000)15,779 acres
(/
(/
.-,
.-,
.-,
(/
Kendrick Fire (1980)185 acres
Slate Fire (1996)379 acres
Horseshoe Fire (1996)8,650 acres
Curley Fire (1980)2,708 acres
Kelly Fire (1971)2,732 acres
Wild Bill Fire (1973)7,814 acres
Kelly Fire (1954)4,582 acres
Burnt Fire (1973)7,316 acres
Hostetter Fire (1950) 1,077 acres(1968) 225 acres
Bear Jaw Fire (1995)780 acres
Hochderffer Fire (1996)16,400 acres
Kendrick Fire (1956)292 acres
Trick Fire (1993)344 acres
White Horse Fire (1967)865 acres
Ft. Valley Fire (1948)2,068 acres
Leroux Fire (2001)1,113 acres
Radio Fire (1977)4,600 acres
Side Fire (1996)320 acres
Power Fire (2000)1,527 acres
Pipe Fire (2000)664 acres
Belle Fire (1951)1,128 acres
A-1 Fire (1950)1,002 acres
Wallace Fire (1979)327 acres
Joe Crouse, Andy Meador, Coconino NF data
NASA Visible EarthCredit:Jacques Descloitres, MODIS Land Rapid Response Team, NASA/GSFCSatellite:TerraSensor:MODISData Start Date:06-30-2002
Arizona 2002
Scar of the Rodeo-Chediski fire
468,638 acres
Does forest structure make a difference?
This is the Trick Fire, 1993, burning near the San Francisco Peaks, AZ
Effects of forest restoration on fire behavior: Grand Canyon, Arizona
Restoration Techniques
• Overstory trees: thinning, species composition, spatial pattern, old-growth.
• Understory herbs and shrubs: natural regeneration, seeding, planting.
• Fuels: accumulated fuels, canopy fuels, dead biomass as nutrient sources and habitat.
• Fire: re-introducing fire, unique initial burn conditions, smoke.
• Monitoring and adapting: evaluating results and making changes.
Covington, W.W., P.Z. Fulé, M.M. Moore, S.C. Hart, T.E. Kolb, J.N. Mast, S.S. Sackett, and M.R. Wagner. 1997. Restoration of ecosystem health in southwestern ponderosa pine forests. Journal of Forestry 95(4):23-29.
Project Progress
• Goal is to reduce uncharacteristically severe wildfire hazard, restore forest structure and dynamics.
• Three experimental blocks measured 1997 (in the snow!)
• Grand Canyon NP: draft EA 1998, protests of “logging in canyon,” no action taken.
• New environmental process completed in 2002 with 5” diameter cap. Thinning completed by Northern Arizona Conservation Corps.
Northern Arizona Conservation Corps members thinning and piling slash with hand tools on Grand Canyon’s North Rim, October, 2002
Experimental Design
• Kaibab National Forest: EA part of “Scott,” thinned 1999, burned fall 1999, remeasured 2000.
• Control: continued fire exclusion.• Three restoration alternatives.• Full restoration: thinning (1.5/3 Rx), fuel
treatment, rx fire.• Minimal thinning: thinning around old-growth
trees, fuels, rx fire.• Burn-only: no fuel treatment, rx fire --
represents current management practice.
Full Restoration
Burn Only
Minimal Thinning
Burned October 1999
Fulé, P.Z., W.W. Covington, H.B. Smith, J.D. Springer, T.A. Heinlein, K.D. Huisinga, and M.M. Moore. 2002. Testing ecological restoration alternatives: Grand Canyon, Arizona. Forest Ecology and Management 170:19-41.
Forest structure influences fire behavior
Crown bulk density
Canopy base height
Fuel model 9 or 10
Fuel model 2 or 9
PRE-Treatment: torching at 21 mph, crowning at 33-40 mph.POST-Treatment (FULL): torching at 35 mph, crowning at 75 mph.
Comparison to reference (1887) fire behavior: torching 42 mph, crowning 55-80 mph
PRE-Treatment Torching and Crowning Indices
0
5
10
15
20
25
30
35
40
45
Control Full Min Burn
Win
ds
pee
d (
mp
h)
Torching IndexCrowning Index
POST-Treatment Torching and Crowning Indices
0
10
20
30
40
50
60
70
80
90
Control Full Min Burn
Win
ds
pe
ed
(m
ph
)
Torching IndexCrowning Index
Treated stand, low density/low fuel
Untreated stand, high density/high fuel
Do model results hold up in real fires?
Rodeo-Chediski fire 2002: White Mountain Apache lands
No treatment, killed by fire
Tree thinning and prescribed burning,survived fire
Rodeo-Chediski Fire, 2002
Treatments 1991-2001, forest above 6,560’, ≤ 45% slope
76% of untreated area burned moderate or high severity
Only 4% (~1000 acres) of cut + burn had high severity
Effects of Treatments
0
10
20
30
40
50
60
70
Cut and Burned Burn Only No Treatment
Per
cen
t o
f F
ire
Are
a
Low
Moderate
High
Future Fires
• Increasing in size, intensity, and severity.
• Increasing fire suppression costs and loss of life.
• Firefighting priorities require focus on urban interface (lives & property) sacrificing wildlands.
• Interaction with climate change: drought & beetles.
Great Basin Incident Mgt Team (above)
forestfire.nau.edu/beetles.htm
Arizona Public Service
University of Arizona
Fuel hazards associated with bark beetle-caused tree mortality in the Southwest.
“The most destructive fire … was fed by more than a million mature pine trees killed over the past year by a bark beetle infestation and drought. The fire front in the national forest was nearly 40 miles long … “John M. Broder, NY Times, October 27, 2003
“Even before the winds came, the risk of fire in Southern California was considered extremely high because several years of drought had left trees vulnerable to the bark beetle and other pests and diseases. Hundreds of thousands of trees are estimated to have died, making them easy to burn.”Andrew Pollack, NY Times, October 27, 2003
Forest Acres Ponderosa
Acres Beetle Attack
Percent Affected
Apache-Sitgreaves
729,306 129,895 18%
Coconino 714,864 60,425 8%
Coronado 6,916 10,255 * 100% +
Kaibab 432,023 6,010 1%
Prescott 50,650 75,580 * 100% +
Tonto 140,128 66,585 48%
* Much of the “piñon/juniper type” forest includes some ponderosa pine. Figures for 2003 from FS Forest Health Protection program.
Pine Bark Beetle Attack