Faculty of Geosciences Copernicus Institute of Sustainable Development Environmental Sciences
Layout: C&M – Faculty of Geosciences – ©2015 (8865)
Stefan C. Dekker 1 , Zun Yin 2 , Mara Baudena 1 , Bart van den Hurk 3 and Henk Dijkstra 2
(1) Utrecht University, Environmental Sciences, Copernicus Institute of Sustainable Development, Utrecht, Netherlands (s.c.dekker@uu.nl), (2) Utrecht University, Institute for Marine and Atmospheric Research,
(3) Royal Netherlands Meteorological Institute de Bilt
Introduction
• Land-atmosphere feedbacks can generate sudden shift in the vegetation state.
• Bimodal distributions of woody cover with mean annual precipitation provide evidence that alternative stable
states may exist 1,2 .
• Understanding clearly the climate conditions behind this bimodality is important to predict crucial transitions due to climate change
Results from Satellite (Modis) data 3
• Bimodality also found with Mean Annual Radiation (Fig.1)
• Cell by cell analyses show only bimodality at boundaries between grassland-savanna and savanna-forest (Fig.2)
• Best prediction of Land Cover is with a combination of Mean Annual Precip, dry season length, and seasonality (Fig. 3)
How do global models represent savannas? 4
• Three Dynamic-Global Vegetetation Models are used to model savanna-forest systems
• Ecological theory: grass-fire feedback is able to simulate bimodality
• Tree-grass fire feedback are differently included in the model
Conclusions
• Bimodality is not observed in current data of woody cover and biomass per grid cell
• Bimodality found with precipitation, radiation and other forcings due to strong correlation between forcing data
• Seasonality is important to predict bimodality
• A bimodal systems can be bistable due to the mechanisms at play: Tree-Grass fire feedback and seasonality are
important
References
1. Staver, A. C., Archibald, S. & Levin, S. A. The Global Extent and Determinants of Savanna and Forest as Alternative Biome States. Sci. 334 , 230–232 (2011).
2. Hirota, M., Holmgren, M., Van Nes, E. H. & Scheffer, M. Global Resilience of Tropical Forest and Savanna to Critical Transitions. Sci. 334 , 232–235 (2011).
3. Yin, Z., Dekker, S. C., M. Van Den Hurk, B. J. J. & Dijkstra, H. a. Bimodality of woody cover and biomass across the precipitation gradient in West Africa. Earth Syst. Dyn. 5, 257–270 (2014).
4. Baudena, M, Dekker S.C.. et al. Forests, savannas and grasslands: bridging the knowledge gap between ecology and Dynamic Global Vegetation Models. Biogeosciences Discuss. 11, 9471–9510 (2014). (in press for BG)
Figure 3 Prediction Land-cover
a. Prediction only with mean annual Precipitation (P) b. Prediction with P and length dry season (LD)
c. Prediction with P, LD, Entropy monthly precip d-f. Difference between 3c and 1a
F, S, G are resp Forest, Savanna and Grass.
s means stable, b means bistable.
‹ Figure 1 a) Map of Woody Cover (W) and b. above ground biomass (B). c,d,e Histograms of W, B and mean annual radiation
Figure 2 Observed bimodality in Woody Cover per gridcell Bimodality of S-F(Savanna-Forest) and G-S (Grass-Savanna) only observed at boundaries. Bimodality criterion with
Integrated Completed likelyhood
20°W 10°W 0°E 10°E 20°E 30°E
5°S0°N5°N10°N15°N20°N
(a)
0.2 0.4 0.6 0.8 W (−)
lat.l
20°W 10°W 0°E 10°E 20°E 30°E
5°S0°N5°N10°N15°N20°N
(b)
2 4 6 8 10 12 14 B (kgC m−2)
fcr
0.0 0.2 0.4 0.6 0.8 1.0
0123
4 (c): W (−)
bior
0 5 10 15
0.000.050.100.15 (d): B (kgC m−2)
180 200 220 240 260
0.0000.0150.030
(e): R (W m−2)
20°W 10°W 0°E 10°E 20°E 30°E
5°S0°N5°N10°N15°N20°N
B G G−S S S−F F
20°W 10°W 0°E 10°E 20°E 30°E
5°S0°N5°N10°N15°N20°N
(a)
20°W 10°W 0°E 10°E 20°E 30°E
5°S0°N5°N10°N15°N20°N
(b)
20°W 10°W 0°E 10°E 20°E 30°E
5°S0°N5°N10°N15°N20°N
(c)
B G
sG
bS
bS
sS
bF
bF
s20°W 10°W 0°E 10°E 20°E 30°E
5°S0°N5°N10°N15°N20°N
(d):Forest
20°W 10°W 0°E 10°E 20°E 30°E
5°S0°N5°N10°N15°N20°N
(e):Savanna
20°W 10°W 0°E 10°E 20°E 30°E
5°S0°N5°N10°N15°N20°N
(f):Grass
−
= +
Figure 4 Model results of JSBach, LPJ-Guess, aDGVM.
All models show water-limitation. Due to negative grass- fire feedbacks, only aDGVM show bistability.
Figure 5 Positve grass-fire feedback (a) explaining observed bimodality in Modis tree cover data (b).
0 20 40 60 80 100
0 20 40 60 80 100
0 20 40 60 80 100
0 500 1000 1500 2000 2500 3000
tree cover (%)tree cover (%)tree cover (%)
mean annual rainfall (mmy−1) A
B
C
grass as fuel
competition tree-grass (light and water)
Grass
A
Savanna Trees
-
Ecological theory & aDGVM
-
- +
Forest Trees
water competition grass-tree seedlings
-
-
- -
- -
Light competition
damage to trees
grass as fuel
competition tree-grass (light and water)
Grass
C
Savanna Trees
-
LPJ-GUESS-SPITFIRE
-
- +
Forest Trees
water competition grass-tree seedlings
-
- competition Light
damage to tree seedlings grass as fuel
Competitive exclusion of trees on grass (light)
Grass
B
Trees
-
JSBACH
-
- +
trees as fuel
+
trees as fuel
+
trees as fuel
+
water use by grass (only transitory)
damage to trees
(a)
0 10 20 30 40 50 60 70 80 90 100
0 500 1000 1500 2000 2500 3000 0 500 1000 1500 2000 2500 3000
mean annual rainfall (mm y−1)
tree cover (%)
mean annual rainfall (mm y−1)
A B
(b)
JSBACH LPJ-Guess-Spitfire aDGVM
Extent Global Global Mainly tropical
Coupled/offline Coupled model Only off line Only off line
Type Vegetation Plant-Funct-Type Individual based Individual based
Length Run CMIP5-run 1850-2005 1960-2007 TRMM CRU
Resolution 1.9° 1° 1.0°
Grass-Fire-Feedback Negative Positive / Negative Positive
Results
Water limitation î Yes Yes Yes
Grass-Tree Competition Trees always outcompete grass At low P grass outcompete grass Grasses better competitors via seedlings
Bimodality No No No
î
0 20 40 60 80 100
0 20 40 60 80 100
0 20 40 60 80 100
0 500 1000 1500 2000 2500 3000
tree cover (%)tree cover (%)tree cover (%)
mean annual rainfall (mmy−1) A
B
C
0 20 40 60 80 100
0 20 40 60 80 100
0 20 40 60 80 100
0 500 1000 1500 2000 2500 3000
tree cover (%)tree cover (%)tree cover (%)
mean annual rainfall (mmy−1) A
B
C
î
0 20 40 60 80 100
0 20 40 60 80 100
0 20 40 60 80 100
0 500 1000 1500 2000 2500 3000
tree cover (%)tree cover (%)tree cover (%)
mean annual rainfall (mmy−1) A
B
C
0 20 40 60 80 100
0 20 40 60 80 100
0 20 40 60 80 100
0 500 1000 1500 2000 2500 3000
tree cover (%)tree cover (%)tree cover (%)
mean annual rainfall (mmy−1) A
B
C
0 20 40 60 80 100
0 20 40 60 80 100
0 20 40 60 80 100
0 500 1000 1500 2000 2500 3000
tree cover (%)tree cover (%)tree cover (%)
mean annual rainfall (mmy−1) A
B
C
î
0 10 20 30 40 50 60 70 80 90 100
0 500 1000 1500 2000 2500 3000 0 500 1000 1500 2000 2500 3000
mean annual rainfall (mm y−1)
tree cover (%)
mean annual rainfall (mm y−1)
A B