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The nonlinear physics of dryland landscapes
Ehud Meron Institute for Dryland Environmental Research & Physics Department
Ben-Gurion University
Squill חצב
Cistanche tubulosaיחנוק Seashore Paspalum
Physics Colloquium, Toronto, March 5, 2009
Motivation Ben G
urio
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, Ehud M
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.bgu.a
c.il/~ehud
Innocent questions such as
how climate changes affect species diversity (bears on ecosystem function and stability) ?are quite complex:
Focusing on the direct response of any individual to the changing climatic conditions is insufficient because of indirect processes at the population and community levels that affect species diversity:Climate change vegetation patterns resource distributions, seed dispersal, consumer pressure species diversity
Climate change inter-specific plant interactions transitions from competition to facilitation species diversity
More generally, environmental changes affect species assemblage properties by inducing indirect processes involving various levels of organization often across different spatial scales.
Mathematical models circumvent these limitations and allow:
1. Identifying asymptotic behaviors (rather than transients).2. Isolating factors and elucidating mechanisms of ecological
processes3. Studying various scenarios of ecosystem dynamics4. Proposing and testing management practices
Laboratory and field experiments are limited by duration, spatial extent and by uncontrollable environmental factors.
Added value of mathematical modeling:
Motivation Ben G
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, Ehud M
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Study processes of this kind by mathematical modeling as a complementary tool to field and laboratory experiments.
Mathematical modeling has its own limitations:
Models simplify the complex reality, quite often oversimplify it
The challenge is to propose simple models that not only reproduce
observed behaviors but also have predictive power – usually requires identifying and modeling basic feedbacks
Outline Ben G
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1. Background:Vegetation patterns, feedbacks between biomass and water, and between above-ground below-ground biomass.
2. Population level: Introduction of a spatially explicit model for a plant population, applying it to vegetation pattern formation along a rainfall gradient and to desertification.
3. Two-species communities: Extending the model to two populations representing speciesbelonging to different functional groups – the woody-herbaceoussystem. Using it to study mechanisms affecting species diversity (not yet community level properties).
4. Many-species communities:Extending the model to include trait-space and use it to derive community level properties such as species diversity along a rainfall gradient.
5. Conclusion
Aerial photograph of vegetation bands in Niger of ‘tiger bush’ patterns on hill slopes (Clos-Arceduc, 1956)
Recent studies: Catena Vol. 37, 1999 Valentin et al. Catena 1999, Rietkerk et al. Science 2004
A worldwide phenomenon observed in arid and semi-arid regions, 50–750 mm rainfall (Valentin et al. 1999)
Background: Vegetation patterns Ben G
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Salt formation in the Atacama desert (Marcus Hauser)
Precipitation
infiltration
(1) Infiltration
Soil crusts reduce infiltration
BiomassBiomass
Water infiltration Water infiltration
Soil waterSoil water
Positive feedback
(2) Root augmentation
BiomassBiomass
Rootextension Rootextension
Water uptakeWater uptake
Positive feedback
Precipitation
Both feedbacks can induce vegetation patterns because they involve water
transport help patch growth but inhibit growth in the patch surroundings
Quantified by an infiltration
contrast parameter cQuantified by a root
augmentation parameter
Background: Biomass-water and below-aboveground feedbacks B
en G
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222
2
2
22
)1(
hhhIhpt
h
wwGLwIht
w
bbbbGt
b
hhh
ww
bb
Gilad et al. (PRL 2004, JTB 2007) [Earlier models: Lefever & Lejeune (1997); Klausmeier, (1999); HilleRisLambers et al. (2000), Okayasu & Aizawa (2001); Von Hardenberg et al. (2001); Rietkerk
et al. (2002); Lejeune et al. (2002); Shnerb et al. (2003)]
Root augmentation as plant grows ~ root to shoot ratio dbdL~
2
2
),(12exp
2
1),,(
trb
rrtrrg
'),'(),,'(),('),'(),',(),( rdtrbtrrgtrGrdtrwtrrgtrG wb
bL 1~
qtrb
cqtrbtrI
),(
/),(),(
Infiltration contrast between
vegetation patch and bare soil
I
c/0 b
c= 1 no contrast
c>>1 high contrast
Population level: a spatially explicit model Ben G
urio
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, Ehud M
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h
Surface-water height
Soil-water content
Biomass
Plain topography
infiltration
Precipitation
Mechanism of migration:
~ 1 cm/yr
Population level: Vegetation states along a rainfall gradient B
en G
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Uniform states:Bare-soil state (b = 0) Fully vegetated state (b 0)
Pattern states: Spots, stripes, gaps
Plane topography:
Slope
Constant slope:
Same uniform statesPattern states: Spots, bands
slope
Dow
nhill
Ben G
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, Ehud M
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Population level: Vegetation states along a rainfall gradient
spot pattern Max(b)
B
SPrecipitation range where
bothbare-soil and spots are stableBistability range for any otherconsecutive pair of states: spots & stripes, stripes & gaps, gaps & uniform vegetaqtion
Multistability of states:
2. Spatially mixed patterns (240, 360)
Mathematically – homoclinic snaking(Knobloch, Nonlinearity 2008).
Equivalent to localized structures in nonlinear optics, fluid dynamics, etc.
Implications:1. Stable localized
structures (120)Squill חצב
http://desert.bgu.ac.il
Ben G
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, Ehud M
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A dynamical-system view of desertification
S
B
Spot pattern
Population level: Vegetation states along a rainfall gradient3. State transitions
The positive feedbacks that induce vegetation patterns are also responsible for the bistability range of bare soil and spots:
The stronger the feedbacks the wider the bistability range and the
less vulnerable to desertification the system is.Many more causes and forms of desertification: gully formation
byerosion, active sand dunes, the human factor, …
Desertification - an irreversible decrease in biological productivity induced by a climate change.
Desertification in the northern Negev
Spots Stripes
Gaps
Stripes of Paspalum vaginatum
Population level: Observations of vegetation patterns Ben G
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Mixed gaps and stripes
Spots
Mixed spots and stripes
Rietkerk
Ben G
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Population level: Observations of vegetation patterns
Barbier
Population level: Soil-water patterns
Strong infiltration Weak augmentation
Strong augmentation Weak infiltration
14m 3.5m 3.5m
Effects of the biomass-water feedbacks:
Infilt
rati
on c
ontr
ast
Root augmentation (water uptake)
Ben G
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C=
10C
=1.
1
Facilitation
Competition
Aridity
stress
222
2
1
2
22
,...,1)1(
hhhIhpt
h
wGwLwIht
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b
hhh
w
n
i
iw
biiiiib
ii
# of functional groups (fg)
Community level: a model for several functional groups B
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Two functional groups: b1 - woody, b2 - herbaceous
Uniform woody
Uniform herbaceous
Spots
b1 b2
b1 b2
b1 b2
b1 b2
Inter-specific interactions along a rainfall gradient:
Community level: Competition vs. facilitation Ben G
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Mechanism:
Infiltration remains high, but uptake drops down because of smaller woody patch.
Ic/0 b
Competition facilitation
Woody-herbaceous system:
Consistent with field observations of annual plant–shrub interactions along an aridity gradient: Holzapfel, Tielbörger, Parag, Kigel, Sternberg, 2006
Facilitation in stressed environments: Pugnaire & Luque, Oikos 2001, Callaway and Walker 1997 Bruno et al. TREE 2003
CompetitionFacilitation
Woody species alone:Ameliorates its micro-environment as aridity increases.
Woody patches can buffer species diversity loss as aridity increases
Woody alone
Downhill
Clear cutting on a slope in a bistability range of spots and bands:
Species coexistence and diversity are affected by global pattern transitions. Coexistence appears as a result of bands spots transition.
Mechanism: spots “see” bare areas uphill twice as long as bands and infiltrate more runoff.
b1
b2
Woody-herbaceous
Community level: Competition vs. facilitation Ben G
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n U
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, Ehud M
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c.il/~ehud
Inter-specific interactions and pattern transitions:
Current form of model cannot provide information about species
assemblage properties such as species diversity.
Large communities Ben G
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Extend the space over which biomass
variables are defined to include a trait subspace
and use this trait space to distinguish amongdifferent species within a functional group.
txBB ,,
physical subspace
trait subspace
1
2
Species A
Species B
1. A single functional group with one-dimensional trait space A simple system:
2. Homogeneous system (no spatial patterns)
Small plants, long rootsBig plants, short roots
Pulse solutions: provide information on species assemblage properties:Width Richness Height Abundance Position
Composition
ξ
B
Small plants, long rootsBig plants, short roots
Deriving community-level properties Ben G
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Stationary pulse solutions at increasing precipitation rates:
Species diversity along a rainfall gradient Ben G
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Precipitation rate
As precipitation rate increases:
1. Species diversity (width) increases2. Abundance (height) increases3. Average composition moves to lower ξ values, i.e. to species
investing more in above-ground biomass and less in roots.
Derive diversity-resource relations
Richness
(herbs)
Precipitation
Herbs onlyIn the presence of Woody patches
Can woody patches buffer species
diversity loss?
Conclusion Ben G
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, Ehud M
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Various aspects of this complexity can be addressed using a single
platform of nonlinear mathematical models that capture basic feedbacks between biomass and water and between above-
groundand below-ground biomass.
Eco-physical phenomena involve various levels of organization, different time scales and different spatial scales. This results in many indirect processes that bear on the questions that we ask, including
Bottom-up processes:
plant interactions vegetation pattern formation
Top-down processes
pattern transitions plant interactions
Theoretical results are consistent with many field observations,
but controlled experiments are needed!
Jost von
Hardenberg
Hezi
Yizhaq
Jonathan
Nathan
Assaf
Kletter
Moshe
shachak
Erez
Gilad
Moran
Segoli Antonello
Provenzale
Efrat
Sheffer
Acknowledgement Ben G
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, Ehud M
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c.il/~ehud
References
Israel Science Foundation
James S. McDonnel Foundation (Complex Systems program)
The Center for Complexity Science
Israel Ministry of Science (Eshcol program)
Funded by: Ben G
urio
n U
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, Ehud M
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c.il/~ehud
1. J. Von Hardenberg, E. Meron, M. Shachak, Y. Zarmi, “Diversity of Vegetation Patterns and Desertification” Phys. Rev. Lett. 89, 198101 (2001).
2. E. Meron, E. Gilad, J. Von Hardenberg, M. Shachak, Y. Zarmi, “Vegetation Patterns Along a Rainfall Gradient”, Chaos Solitons and Fractals 19, 367 (2004).
3. E. Gilad, J. Von Hardenberg, A. Provenzale, M. Shachak, E. Meron, “Ecosystem Engineers: From Pattern Formation to Habitat Creation”, Phys. Rev. Lett. 93, 098105 (2004).
4. H. Yizhaq, E. Gilad, E. Meron, “Banded vegetation: Biological Productivity and Resilience”, Physica A 356, 139 (2005).
5. E. Meron & E. Gilad, “Dynamics of plant communities in drylands: A pattern formation approach”, in Complex Population Dynamics: Nonlinear Modeling in Ecology, Epidemiology and Genetics, B. Blasius, J. Kurths, and L. Stone, Eds. , World-Scientific, 2007.
6. E. Gilad, J. Von Hardenberg, A. Provenzale, M. Shachak, E. Meron, “A mathematical Model for Plants as Ecosystem Engineers”, J. Theor. Biol. 244, 680 (2007).
7. E. Gilad, M. Shachak, E. Meron, “Dynamics and spatial organization of plant communities in water limited systems” , Theo. Pop. Biol. 72, 214-230 (2007).
8. E. Meron, E. Gilad, J. Von Hardenberg, A. Provenzale, M. Shachak, “Model studies of Ecosystem Engineering in Plant Communities”, in Ecosystem Engineers: Plants to Protists , Eds: K. Cuddington et al., Academic Press 2007.
9. E. Sheffer E., Yizhaq H., Gilad E., Shachak M. and & Meron E., “Why do plants in resource deprived environments form rings?” Ecological Complexity 4, 192-200 (2007).
10. E. Meron, H. Yizhaq and E. Gilad E., “Localized structures in dryland vegetation: forms and functions”, Chaos 17, 037109 (2007)
11. Kletter A., von Hardenberg J., Meron E., Provenzale A., "Patterned vegetation and rainfall intermittency", J. Theoretical Biology 2008.
12. Shachak M., Boeken B., Groner E., Kadmon R., Lubin Y., Meron E., Neeman G., Perevolotsky A., Shkedy Y. and Ungar E., " Woody Species as Landscape Modulators and their Effect on Biodiversity Patterns", BioScience 58, 209-221 (2008).
References Ben G
urio
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, Ehud M
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Biological soil crusts
Karnieli
Soil crust
Areal photographs Egypt-Israel border
Ben G
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, Ehud M
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c.il/~ehud
Ben G
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, Ehud M
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Desertification induced by drought
Remains of a spot pattern of Noaea mucronata in the northern Negev
Moshe Shachak (2009)