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Invasive Plants that
Alter Fire Regimes in the
Deserts of North America
Matt Brooks
U.S. Geological Survey
Western Ecological Research Center
Yosemite Field Station, El Portal CA
Jeanne Chambers
U.S.D.A. Forest Service
Rocky Mountain Research Station
Reno NV
Presentation Outline
• Explain what a fire regime is and how
invasive plants can alter it.
• Describe how fire regimes are altered in
major desert vegetation types.
• Present recommendations on how best to
manage altered fire regimes.
Fire Regimes
• Time (seasonality, return interval)
• Space (size, complexity)
• Magnitude (intensity, severity, type)
It is relatively simple to comprehend the characteristics
and effects of an individual fire. However, it is much more
difficult to do the same for fire regimes, which are defined
as patterns of burning across time, space, and magnitude.
Sugihara et al. 2006
Fire Regimes
Fire regimes can be strong forces in the evolution of
species traits. When fire regimes are rapidly altered,
individual species and species assemblages may be
significantly affected.
photo by Lesley DeFalco
Plants
Fuels
Fire Regime
Climate Topography
Nonnative Plants
Fuels
Fire Regime
Native Plants
Climate Topography
Nonnative Plants
Fuels
Fire Regime
Native Plants
+ –
–
Brooks et al. 2004
Invasive Plant / Fire Regime Cycle
Determining that an invasive plant/fire
regime cycle has become established
1. Plant invasion has changed fuel structure
and fire behavior
2. The invasive species benefit from these
changes, often to the detriment of natives
3. These changes lead to an altered fire regime
- this last step can be very difficult to document
- must show a change in some fire regime factor
Brooks 2008
Nonnative PlantsAnnual grassland
(dominated by Bromus spp.)
Fuels↓ Coarse load
↑ Fine load
↑ Continuity
↑ Ignitability
Fire Regime↑ Frequency
↑ Extent
↑ Seasonal window
Native PlantsSagebrush-steppe, Blackbrush,
Creosotebush scrub
+ –
–
Grass / Fire Cycle
in Hot and Cold Desert Shrublands of North America
adapted from Brooks 2008
Resiliency of Non-native Grasses and
Native Perennials Following Fire
Non-native grasses have high resiliency to fire.
Cover of Perennial Plants
fire history (times burned 1984-1993)
0 1 2 3
cover
(%)
0
5
10
15
20
25
30
Bromus rubens Above-Ground Live Biomass
recurrent fire (times burned 1984-1993)
0 1 2 3
dry
kg/h
a
0
100
200
300
400
500
600
700
800
900
Biomass of Non-native Grasses
Native perennials have low resiliency to fire
Cover of Native Perennials
fire history (times burned 1984-1993)
0 1 2 3
sp
ecie
s r
ichn
ess (
# o
f spe
cie
s)
0
2
4
6
8
600 m2 scale
0
2
4
6
8
10
12
60 m2 scale
Species Richness of Native Perennials
Brooks in prep
Annual grasses invading desert shrublands
• Perennial shrubs are gone
• Landscape has low resistance to
fire
• Annual grasses and other non-
natives are the dominant species
left and are resilient to fire
Invading PlantsMesquite, Tarbush, creosotebush
Fuels↓ Fine surface fuels
↑ Coarse canopy fuels
↓ Ignitability
Fire Regime↓ Frequency
↑ Intensity
↓ Seasonal window
Surface fire to crown fire
Native PlantsPerennial grasses
+ –
–
Woody Plant / Fire Suppression Cycle in
Hot Desert Grasslands of North America
adapted from Brooks 2008
Woody plants invading hot desert grasslands
• Perennial grasses are gone
• Landscape has high
resistance to fire
• Woody species are the
dominant species left to
recover if a fire happens to
occur
adapted from MacMahon and Wagner 1985
Sonoran
annual precipitation (cm)
% d
uring w
inte
r
0
100
50
10 3020 40
Mojave
Chihuahuan
woody perennials
perennial grasses
increasing productivity
Great Basin
50
Deserts of North America
Sonoran
annual precipitation (cm)
% d
uring w
inte
r
0
100
50
10 3020 40
Mojave
Chihuahuan
Great Basin
50
Native vegetation insufficient to
fuel historical fires
Native vegetation sufficient to
fuel historical fires
Deserts of North America
annual precipitation (cm)
% d
uring w
inte
r
0
100
50
10 3020 40
Cold Desert Shrublands
50
Native vegetation insufficient to
fuel historical fires
Native vegetation sufficient to
fuel historical fires
Deserts of North America
Hot Desert
Shrublands
Hot Desert Grasslands
annual precipitation (cm)
% d
uring w
inte
r
0
100
50
10 3020 40 50
Native vegetation insufficient to
fuel historical fires
Native vegetation sufficient to
fuel historical fires
Deserts of North America
Riparian
Riparian
Riparian
Riparian
Hot Desert Shrublands
Low elevation shrubland
Middle elevation shrubland
High elevation shrubland/woodland
Brooks and Minnich 2006
Low
elevation
Middle
elevation
High
elevation
Low
elevation
Middle
elevation
High
elevation
Current Hot Desert Shrubland Fire Regimes
Non-native Annual Fuel Regime
– Driven by single- or consecutive-year rainfall
patterns causing episodic fine fuel buildup (e.g. due
to ENSO)
– Low and middle elevations where native woody
fuels are typically too sparse to carry fire
– Fires were historically rare to non-existent and
native vegetation has low resiliency to fire
– Significant fire management intervention may be
warranted to break the invasive plant / fire regime
cycle
Brooks in prep
Current Hot Desert Shrubland Fire Regimes
Native Perennial Fuel Regime
– Driven by decade and century scales of rainfall
patterns causing gradual woody fuel buildup (e.g.
due to PDO)
– High elevations where native woody fuels can carry
fire
– Fires occurred historically and native vegetation has
some resiliency to fire
– Fire suppression may be warranted at the WUI, but
on a landscape scale periodic fire on 75-100+ years
intervals may be desirable
Brooks in prep
Cold Desert Shrublands
Woodland
10-20+
Salt Desert Shrub
4 – 7”
Sagebrush steppe
7-16”
• Historically, salt desert shrublands
(mostly chenopods) rarely if ever
burned.
• In sagebrush types (Artemisia
species), fire return intervals were
moderate to long (~50 to 200++
yrs) depending on precipitation/
productivity. Fire size and
patchiness were variable.
• Pinyon and juniper woodlands were
largely restricted to “fire safe” sites
on ridge tops and steep slopes.PJ woodland
10-20+”
Low to Mid Elevations• Invasive annual grasses (cheatgrass, red
brome, medusa head) were introduced in late 1800s and rapidly spread. Increase in flammable fine fuels with high rate of spread.
Initiation of annual grass fire cycle -
shorter FRIs, larger, more contiguous fires
Other Factors - longer and more severe fire
seasons, more human fire starts
High Elevations
• Overgrazing by livestock beginning in mid-late
1800s decreased native perennial grasses and
forbs (fine fuels).
• Decreased competition from herbs, favorable
establishment conditions and fire reduction led
to increases in shrubs and pinyon and juniper
(woody fuels).
Less frequent fires until last decades –
increased fire size and severity since then
Altered Fire Regimes and
Invasive Species
• High severity fire and factors that deplete
herbaceous understory species increase
susceptibility to invasion.
• Chambers et al. (2007) found effects on
cheatgrass biomass and seed production
are additive:– Herb Removal = 2 to 3 fold increase
– Fire = 2 to 6 fold increase
– Herb Removal + Fire = 10 to 30 fold increase
Resistance to cheatgrass and resilience or
recovery after fire is increased by perennial
grasses and forbs
Recently, secondary weeds are spreading
through region (knapweeds, yellow star
thistle, rush skeletonweed).
Altered Fire Regimes and
Invasive Species
2003
No. S
eeds/P
lant
020406080
100120140160180
2002
Bio
mass/p
lant (g
)
0.00.20.40.60.81.01.21.4
Undershrub
Interspace
7800'7180'6400'
100%
50%
0%
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50%
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Burn Control Burn Control Burn Control
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2003
No
. S
eed
s/P
lan
t
020406080
100120140160180
2002
Bio
ma
ss/p
lan
t (g
)
0.00.20.40.60.81.01.21.4
Undershrub
Interspace
7800'7180'6400'
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50%
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50%
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Burn Control Burn Control Burn Control
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Burn Control Burn Control Burn Control
How might future increased temperatures
hot and cold desert fire regimes?
• Climatic models predict increasing temperatures.
• Increasing temperatures may drive cold desert conditions more towards hot deserts (e.g. more extreme fire weather conditions and lower live fuels moistures).
• Conditions in higher elevation and more mesic shrublands may become more conducive to dominance by non-native grasses and the grass/fire cycle, and reduced resistance and resiliency of native vegetation to fire.
Brooks and Matchett in prep
How might future changes in precipitation affect
hot and cold desert shrubland fire regimes?
Brooks and Matchett in prep
• Potential future precipitation is much more difficult to predict than temperature.
• Proportions of summer:winter and rainfall:snow, in addition to increases or decreases and interannual variations, all have differing implications for invasive plants, fire regimes, and interactions between the two.
• Increasing temperatures will mean increasing evapo-transpiration rates, so increased rainfall may still lead to decreased soil moisture and concomitant effects on fine and woody fuels.
Hot Desert Grasslands
• Historically, most hot desert grasslands burned at an
average return interval of 5-15 years (range of 2-30 years).
• Fires typically occurred at the beginning on the monsoon
season in late June to early July.• Most woody species are killed by
fire and don’t reproduce until they
are >10 years old.
• Most perennial grasses survive fire
and only have reduced productivity
for a few years.
• As a result, perennial grasses
dominate landscapes that are
burned about every decade.Brooks and McPherson 2008
Hot Desert Grasslandspost-settlement
• Livestock grazing has reduced fire fuel loads to the point that fires cannot spread even under extreme fire weather conditions.
• Fire suppression activities and landscape scale fuel fragmentation from roads have further reduced the amount of area burned.
• As a result, fire return intervals have increased, woody plants have established, and perennial grasses and other herbaceous species have declined, converting grasslands to shrublands.
Brooks and McPherson 2008
Hot Desert Grasslandspost-settlement
• Fires have been reintroduced in an effort to convert
shrublands back to grasslands.
• However fire is typically applied in March or April, outside
of the historical summer fire season.
• While these may favor grasses over shrubs, early-season
fires tend to favor the dominance of a widespread non-
native perennial grass (Lehmann lovegrass), which leads
to low diversity vegetation stands.
Brooks and McPherson 2008
• Historically, FRIs of desert riparian areas likely were influenced by drought, lightning strikes, FRIs of the surrounding landscape, and Native Americans, but in most cases were probably very long.
• Fire size and patchiness were influenced by fuel and fire characteristics, geomorphic setting, and hydrologic regime.
Desert Riparian Ecosystems
• Tamarisk (8 Tamarix sp.) and Russian olive (Elaeagnus angustifolia) were introduced in 1800s.
• Altered flow regimes resulted in drier floodplain environments where the more drought tolerant invaders are replacing native cottonwoods and willows.
• Floods that provided conditions for native species establishment and cleared live and dead vegetation are suppressed.
• Tamarisk and Russian olive now form dense thickets of contiguous fuels with high amounts of woody debris and leaf litter, and create volatile fuel ladders under native cottonwoods.
Fires of higher severity now occur every 10 to 20 years in some riparian areas (Lovich et al. 1994).
Altered Fire Regimes and
Invasive Species
• Tamarisk resprouts after fire, and both invaders have longer-lived seeds and less specific establishment requirements than native cottonwoods and willows.
• Established native vegetation can suppress tamarisk seedlings and decrease susceptibility to invasion (Sher et al 2000, 2002).
Changes in flow regimes have increased both flammability of riparian areas and the spread of invaders
Fires have replaced floods as the primary disturbance in many southwestern riparian ecosystems
Altered Fire Regimes and
Invasive Species
Breaking Invasive Plant / Fire Cycles
Must manage both the invasion process and the fire
regime at landscape scales
• Managing for more desirable FRIs requires maintaining or
increasing ecosystem resistance to invasion and
ecosystem resilience or the ability to recover after fire
• Inherent differences exist in resistance and resilience
among desert vegetation types
– Abiotic and biotic characteristics
– Current ecological conditions
• Management activities need to consider likely FRIs for
target vegetation types and current ecological conditions
Effective Management Hinges on
Resistance and Resilience to FireFactors that decrease resistance and resilience
• Low and highly variable precipitation
• High resource fluctuations due to variable precipitation and fire
• Low abundance and life form diversity of native species
• Transformer species present as adults or propagules
• Abundant and contiguous woody or fine fuels
Low resistance & resilience - hot desert shrub, salt desert, Wyoming sage
Moderate resistance & resilience – mid to high elevation sage, mountain brush
Prevention of Altered Fire Regimes
Routinely assess current ecological conditions to prioritize areas for
management.
Increase resistance in areas with intact native communities
• Prevent and minimize the size of wildfires
• Control invasion vectors and corridors (roads, trails, etc.)
• Eliminate/reduce ongoing stressors (repeated fire, overgrazing)
• Increase early detection and eradication efforts
Increase resilience in areas with intact native communities
• Decrease woody fuel loads if appropriate
• Seed with native species if appropriate
• Actively manage to minimize invasion and stressors
• Minimize other stressors both before and after fire
Restoration of Areas with Altered Fire Regimes
Increase resistance and resilience of transitional or converted
vegetation stands in high priority management areas (e.g. near
intact native vegetation stands, areas of high resource value, the
WUI)
• Use an integrated management approach
– Eliminate or reduce invader abundance and propagule supply
– Restore native species in areas where necessary and feasible
– Create communities with high resilience and desirable FRI
if necessary
• Actively manage to minimize invasion, disturbance, and stressors
Adaptive Management
• Monitor changes occurring and results of management activities
– Link into new regional efforts like NEON and the new UNR and USGS climate change networks
• Use an adaptive management approach focused at landscape scales
– Base on feedback from resource assessments and monitoring
Promote active and effective collaboration among all
stakeholders