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Using empirical and mechanistic models to predict crop
suitability and productivity in climate change research
Anton Eitzinger A.Eitzinger@cgiar.org
P. Laderach, C. Navarro, B. Rodriguez
Decision and Policy Analysis DAPA, CIAT Nairobi, June 13th 2013
Why crop modeling in climate change?
… assessing the impact of climate change on
productivity and climate-suitability of crops and
production systems … and understand the limiting
factors
… using well-established empirical and mechanistic
models such as Ecocrop, Maxent, DSSAT, …..
that allow for the incorporation of spatial data and
fine-tuned biophysical data
How?
Stations by
variable:
• 47,554
precipitation
• 24,542
tmean
• 14,835
tmax y tmin
Sources:
•GHCN
•FAOCLIM
•WMO
•CIAT
•R-Hydronet
•Redes nacionales
-30.1
30.5
Mean annual
temperature (ºC)
0
12084
Annual
precipitation (mm)
B
PREC
• Generate
interpolated climate
surfaces using
ANUSPLIN-SPLINA
with weather station
data
• Cross validating (25
iterations
• uncertainty
TMP
Uncertainty of climate data and models
B
Validation of climate surface (25 iterations)
B
Compare original worldclim with interpolated
GCMs are the only way
we can predict the future
climate
Using the past to learn
for the future
GCM “Global Climate Model”
The Delta Method
• Use anomalies and discard baselines
in GCMs
– Climate baseline: WorldClim
– Used in the majority of studies
– Takes original GCM timeseries
– Calculates averages over a baseline and
future periods (i.e. 2020s, 2050s)
– Compute anomalies
– Spline interpolation of anomalies
– Sum anomalies to WorldClim
Climate data
• For current climate (baseline)
we used historical climate data from WorldClim
www.worldclim.org
• Future climate: global climate models (GCMs)
from IPCC (AR5) – SRES A2, A1B, ..
• Downscaling to provide higher-resolution (2.5 arc-
minutes ~ 5 kilometer)
http://ccafs-climate.org
EcoCrop
The database was developed 1992 by the Land and Water
Development Division of FAO (AGLL) as a tool to identify plant species
for given environments and uses, and as an information system
contributing to a Land Use Planning concept.
In October 2000 Ecocrop went on-line under its own URL
www.ecocrop.fao.org. The database now held information on more
than 2000 species.
In 2001 Hijmans developed the basic mechanistic model (also named
EcoCrop) to calculate crop suitability index using FAO Ecocrop
database in DIVA GIS.
In 2011, CIAT (Ramirez-Villegas et al.) further developed the model,
providing calibration and evaluation procedures.
open
Suitability modeling with Ecocrop
EcoCrop, originally by Hijman et al. (2001), was further developed, providing calibration and
evaluation procedures (Ramirez-Villegas et al. 2011).
It evaluates on monthly basis if there
are adequate climatic conditions
within a growing season for
temperature and precipitation…
…and calculates the climatic suitability of the
resulting interaction between rainfall and
temperature…
How does it work?
• database held information on more than 2000
species
What happens when Ecocrop model runs?
1
2
3
4
5
6
7
8
9
10
11
12
1 kilometer grid cells
(climate environments)
The suitability of a location (grid cell) for a crop
is evaluated for each of the 12 potential
growing seasons.
Growing season
0 24 100 80
For temperature suitability
Ktmp: absolute temperature that will kill the plant
Tmin: minimum average temperature at which the plant will grow
Topmin: minimum average temperature at which the plant will grow optimally
Topmax: maximum average temperature at which the plant will grow optimally
Tmax: maximum average temperature at which the plant will cease to grow
For rainfall suitability
Rmin: minimum rainfall (mm) during the growing season
Ropmin: optimal minimum rainfall (mm) during the growing season
Ropmax: optimal maximum rainfall (mm) during the growing season
Rmax: maximum rainfall (mm) during the growing season
Length of the growing season
Gmin: minimun days of growing season
Gmax: maximum days of growing season
• Growing season: xx days (average of Gmin/Gmax)
• Temperature suitability (between 0 – 100%)
• Rainfall suitability (between 0 – 100%)
• Total suitability = TempSUIT * RainSUIT
If the average minimum temperature in one of these months is 4C or less above Ktmp, it is
assumed that, on average, KTMP will be reached on one day of the month, and the crop will die.
The temperature suitability of that month is thus 0%. If this is not the case, the temperature
suitability is evaluated for that month using the other temperature parameters.
The overall temperature suitability of a grid cell for a crop, for any growing season, is the lowest
suitability score for any of the consecutive number of months needed to complete the growing
season
The evaluation for rainfall is similar as for temperature, except that there is no “killing” rainfall and
there is one evaluation for the total growing period (the number of months defined by Gmin and
Gmax) and not for each month.
The output is the highest suitability score (percentage) for a growing season starting in any month
of the year.
(climate) Suitability modelling
A1B / 2030current
current A1B / 2030
(climate) Suitability modelling
Change in climate-suitability
“assumptions on regional level”
losses gains
Change in climate-suitability Losses
gains
• Maximum entropy methods are very general ways to predict probability
distributions given constraints on their moments
• Predict species’ distributions based on environmental covariates
What is Entropy Maximization?
• You can think of Maxent as having two parts: a constraint
• component and an entropy component
• The output is a probability distribution that sums to 1
• For species distributions this gives the relative probability of observing
the species in each cell
• Cells with environmental variables close to the means of the presence
locations have high probabilities
MaxEnt model
B
21
Input: Crop evidence (GPS points)
19 bioclimatic variables of current (worldclim) & future climate
Output:
Probability of distribution of coffee (0 to 1)
MaxEnt model
Bioclimatic variables for suitability modeling
• Bio1 = Annual mean temperature
• Bio2 = Mean diurnal range (Mean of monthly (max temp - min temp))
• Bio3 = Isothermality (Bio2/Bio7) (* 100)
• Bio4 = Temperature seasonality (standard deviation *100)
• Bio5 = Maximum temperature of warmest month
• Bio6 = Minimum temperature of coldest month
• Bio7 = Temperature Annual Range (Bio5 – Bi06)
• Bio8 = Mean Temperature of Wettest Quarter
• Bio9 = Mean Temperature of Driest Quarter
• Bio10 = Mean Temperature of Warmest Quarter
• Bio11 = Mean Temperature of Coldest Quarter
• Bio12 = Annual Precipitation
• Bio13 = Precipitation of Wettest Month
• Bio14 = Precipitation of Driest Month
• Bio15 = Precipitation Seasonality (Coefficient of Variation)
• Bio16 = Precipitation of Wettest Quarter
• Bio17 = Precipitation of Driest Quarter
• Bio18 = Precipitation of Warmest Quarter
• Bio19 = Precipitation of Coldest Quarter
derived from monthly temperature & precipitation
Coffee suitability - Maxent Results Nicaragua
B
Results
Variable Adjusted
R2
R2 due to
variable
% of total
variability
Present
mean
Change by 2050s
Locations with decreasing suitability (n=89.8 % of all observations)
BIO 14 – Precipitación del mes más seco 0.0817 0.0817 24.8 24.49 mm -3.27 mm
BIO 04 – Estacionalidad de temperatura 0.1776 0.0959 29.1 0.83 0.166
BIO 12 – Precipitación anual 0.2057 0.0281 8.5 2462.35 mm -24.31 mm
BIO 11 - Temperatura media del cuarto más frío 0.2633 0.0576 17.5 20.11 ºC 1.86 ºC
BIO 19 - Precipitación del cuarto más frío 0.2993 0.0155 4.7 169.13 mm -7.08 mm
BIO 05 - Temperatura máxima del mes más cálido 0.3198 0.0102 3.1 28.45 ºC 2.30 ºC
BIO 13 - Precipitación del mes más húmedo 0.2838 0.0205 6.2 450.27 mm 10.72 mm
Otros - - 6.2
Coffee suitability - Maxent Results Nicaragua
B
a Average of Q1 of GCMs
b Average of GMSs
c Average of Q3 of GCMs
d Measure of agreement of
models
e standard deviation of GCMs
b
c
e
Uncertainty of model output (Maxent) using 19 GCMs SRES A2 – timeserie 2040 – 2069 (2050)
Decision Support System for Agro technology Transfer (DSSAT)
+
• For 2 DSSAT-varieties (IB0006 ICTA-Ostua, IB0020 BAT1289
– “INTA Fuerte Sequia”, “INTA Rojo”, and “Tío Canela 75” originating from Nicaragua
– “ICTA Ostua” and “ICTA Ligero” originating from Guatemala
– “BAT 304” originating from Costa Rica
– “SER 16”, SEN 56”, “NCB 226”, and “SXB 412” originating from CIAT, Colombia.
• Sowing on:
– Primera (Beginning of June)
– Postrera (Beginning of September)
• After recollecting data during 2011
results will be used
in a post-project-analysis
to calibrate 2 initial DSSAT varieties
run it again for trial sites and find
spatial and temporal analogues
Accompanying field trials in 5 countries to calibrate DSSAT
Planting date: Between 15th of April and 30th of June1
Variety 1: IB0006 ICTA-Ostua Variety 2: IB0020 BAT1289
Soil 1: IB00000005 (generic medium silty loam) Soil 2: IB00000008 (generic medium sandy loam)
Fertilizer 1: 64 kg / ha 12-30-0 6 to 10 days after germination and 64 kg / ha Urea (46% N) at 22 to
25 days after germination. Fertilizer 2: 128 kg/ha 18-46-0 Fertilizer application on sowing and 64
kg/ha UREA at 22 to 30 days after germination.
Weather data input:
Current climate
Average of 99 MarkSim
daily outputs
Future climate
Ensemble of 19GCM & 99
MarkSim outputs for 2020
& 2050
Runs: 17,800 points x 3
climates x 99 MarkSim-
samples x 8 trials
DSSAT “Tortillas on the Roaster” in Central America
Results: yield change for year 2020 (Primera) – 8 trials
Trial 3 – high performance / high impact
Variety 1: ICTA-Ostua
Soil 1: generic medium silty loam
Fertilizer 2: 128 kg/ha 18-46-0 Fertilizer application on sowing
and 64 kg/ha UREA at 22 to 30 days after germination
Trial 7 – medium high performance / less impact
Variety 1: ICTA-Ostua
Soil 2: generic medium sandy loam
Fertilizer 2: 128 kg/ha 18-46-0 Fertilizer application on sowing
and 64 kg/ha UREA at 22 to 30 days after germination
Statistical negative and positive outliers of predicted yield change by 2020
31
Areas where the production systems of crops can be
adapted
Adaptation-Spots
Focus on adaptation of production system
Areas where crop is no longer an option
Hot-Spots
Focus on livelihood diversification
New areas where crop production can be established
Pressure-Spots
Migration of agriculture – Risk of deforestation!
Identifying Impact-Hot-Spots and select sites for socio-economic analysis
32
• Beans as most important income (sell 70% of harvest)
• Climate variability (intense rain, drought), missing labor & credits,
high input costs, … forces them to changes
• Increasing livestock displace crops into hillside areas
• Half of farmer rent their land
• Distance to market is far
• Mostly no road access in rainy season
• They buy inputs/sell produce from/to farm-stores
(they call them: Coyotes)
Result: Sample-site 1 - Texistepeque (Las Mesas), Santa Ana ,El Salvador
Message 2: Adaptation Strategies must be fine-tuned at each site!
Las Mesas
Altitude: 667 m
(about 2188 feet)
Hot-spot -141 kg/ha
For 2020:
• 35 mm less rain (current 1605mm)
• mean temperature increase 1.1 C
For 2050:
• 73mm less rain ( -5%)
• mean temperature increase 2.3 C
• hottest day up to 35 C (+ 2.6 C)
• coolest night up to 17.7 C (+ 1.8 C)
Hot-spot
33
Message 3: There can be winners if they adapt quickly!
Result: Sample-site 2 – Valle de Jamastran, Danlí, Honduras Adaptation-spot
Jamastran
Altitude: 783 m
(about 2568 feet)
Adaptation-spot -
115 kg/ha
• Active communities with already advanced agronomic
management of maize-bean crops
• Favorable soil conditions and management
• Long-term technical assistance / training
• Irrigation schemes (e.g. 50 mz of 17 bean producers)
• Diversification options (vegetables, livestock)
• Market channels through processing industries
• Advanced infrastructure (electricity, roads)
• Need to optimize water use efficiency
• Credit problems
For 2020:
• 41 mm less rain (current 1094 mm)
• mean temperature increase 1.1 C
For 2050:
• 80 mm less rain ( -7%)
• mean temperature increase 2.4 C
• hottest day up to 34.2 C (+ 2.6 C)
• coolest night up to 17 C (+ 2.1 C)
Decision support system modelling (for benchmark sites)
Agronomic management
Expert & farmer survey
Integrated crop-soil modeling
160 LDSF sample sites
Baseline
domains
Impact
2030 A1b
Experimental
[n] cultivars
[n] fertilizer application
[n] seasons
Application domains
Analysis of biophysical systems and simulating crop yield in relation to management factors. Combine these
models with field observations that allow adjustment of the models in the course of the growing season .
Future
24 GCM
A1B (IPCC)
Current
worldClim
Validation with
available station data
Daily weather generator
MarkSIM
Weather
station data
(daily)
Climate data
yield
soil management
• Downscaling is inevitable.
• Continuous improvements are
being done
• Strong focus on uncertainty
analysis and improvement of
baseline data
• We need multiple approaches to improve the
information base on climate change scenarios
 Development of RCMs (multiple: PRECIS not enough)
 Downscaling empirical, methods Hybrids
 We tested different methodologies
Conclusions climate data
Conclusions crop models
• Ecocrop, when there is a lack on
crop information, for global or
regional assessment
• Maxent, perennial crops with
presence only data (coordinates)
available
• DSSAT, only for few crops (beans,
maize, …), high data input demand
and calibrated field experiments are
necessary
• We need to communicate
uncertainty of model predictions
Empirical
models
Mechanistic
models

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Using empirical and mechanistic models to predict crop suitability and productivity in climate change research

  • 1. Using empirical and mechanistic models to predict crop suitability and productivity in climate change research Anton Eitzinger A.Eitzinger@cgiar.org P. Laderach, C. Navarro, B. Rodriguez Decision and Policy Analysis DAPA, CIAT Nairobi, June 13th 2013
  • 2. Why crop modeling in climate change? … assessing the impact of climate change on productivity and climate-suitability of crops and production systems … and understand the limiting factors … using well-established empirical and mechanistic models such as Ecocrop, Maxent, DSSAT, ….. that allow for the incorporation of spatial data and fine-tuned biophysical data How?
  • 3. Stations by variable: • 47,554 precipitation • 24,542 tmean • 14,835 tmax y tmin Sources: •GHCN •FAOCLIM •WMO •CIAT •R-Hydronet •Redes nacionales -30.1 30.5 Mean annual temperature (ºC) 0 12084 Annual precipitation (mm)
  • 4. B PREC • Generate interpolated climate surfaces using ANUSPLIN-SPLINA with weather station data • Cross validating (25 iterations • uncertainty TMP Uncertainty of climate data and models
  • 5. B Validation of climate surface (25 iterations)
  • 6. B Compare original worldclim with interpolated
  • 7. GCMs are the only way we can predict the future climate Using the past to learn for the future GCM “Global Climate Model”
  • 8. The Delta Method • Use anomalies and discard baselines in GCMs – Climate baseline: WorldClim – Used in the majority of studies – Takes original GCM timeseries – Calculates averages over a baseline and future periods (i.e. 2020s, 2050s) – Compute anomalies – Spline interpolation of anomalies – Sum anomalies to WorldClim
  • 9. Climate data • For current climate (baseline) we used historical climate data from WorldClim www.worldclim.org • Future climate: global climate models (GCMs) from IPCC (AR5) – SRES A2, A1B, .. • Downscaling to provide higher-resolution (2.5 arc- minutes ~ 5 kilometer) http://ccafs-climate.org
  • 10. EcoCrop The database was developed 1992 by the Land and Water Development Division of FAO (AGLL) as a tool to identify plant species for given environments and uses, and as an information system contributing to a Land Use Planning concept. In October 2000 Ecocrop went on-line under its own URL www.ecocrop.fao.org. The database now held information on more than 2000 species. In 2001 Hijmans developed the basic mechanistic model (also named EcoCrop) to calculate crop suitability index using FAO Ecocrop database in DIVA GIS. In 2011, CIAT (Ramirez-Villegas et al.) further developed the model, providing calibration and evaluation procedures.
  • 11. open Suitability modeling with Ecocrop EcoCrop, originally by Hijman et al. (2001), was further developed, providing calibration and evaluation procedures (Ramirez-Villegas et al. 2011). It evaluates on monthly basis if there are adequate climatic conditions within a growing season for temperature and precipitation… …and calculates the climatic suitability of the resulting interaction between rainfall and temperature… How does it work?
  • 12. • database held information on more than 2000 species
  • 13. What happens when Ecocrop model runs? 1 2 3 4 5 6 7 8 9 10 11 12 1 kilometer grid cells (climate environments) The suitability of a location (grid cell) for a crop is evaluated for each of the 12 potential growing seasons. Growing season 0 24 100 80
  • 14. For temperature suitability Ktmp: absolute temperature that will kill the plant Tmin: minimum average temperature at which the plant will grow Topmin: minimum average temperature at which the plant will grow optimally Topmax: maximum average temperature at which the plant will grow optimally Tmax: maximum average temperature at which the plant will cease to grow For rainfall suitability Rmin: minimum rainfall (mm) during the growing season Ropmin: optimal minimum rainfall (mm) during the growing season Ropmax: optimal maximum rainfall (mm) during the growing season Rmax: maximum rainfall (mm) during the growing season Length of the growing season Gmin: minimun days of growing season Gmax: maximum days of growing season
  • 15. • Growing season: xx days (average of Gmin/Gmax) • Temperature suitability (between 0 – 100%) • Rainfall suitability (between 0 – 100%) • Total suitability = TempSUIT * RainSUIT If the average minimum temperature in one of these months is 4C or less above Ktmp, it is assumed that, on average, KTMP will be reached on one day of the month, and the crop will die. The temperature suitability of that month is thus 0%. If this is not the case, the temperature suitability is evaluated for that month using the other temperature parameters. The overall temperature suitability of a grid cell for a crop, for any growing season, is the lowest suitability score for any of the consecutive number of months needed to complete the growing season The evaluation for rainfall is similar as for temperature, except that there is no “killing” rainfall and there is one evaluation for the total growing period (the number of months defined by Gmin and Gmax) and not for each month. The output is the highest suitability score (percentage) for a growing season starting in any month of the year.
  • 17. current A1B / 2030 (climate) Suitability modelling
  • 18. Change in climate-suitability “assumptions on regional level” losses gains
  • 20. • Maximum entropy methods are very general ways to predict probability distributions given constraints on their moments • Predict species’ distributions based on environmental covariates What is Entropy Maximization? • You can think of Maxent as having two parts: a constraint • component and an entropy component • The output is a probability distribution that sums to 1 • For species distributions this gives the relative probability of observing the species in each cell • Cells with environmental variables close to the means of the presence locations have high probabilities MaxEnt model
  • 21. B 21 Input: Crop evidence (GPS points) 19 bioclimatic variables of current (worldclim) & future climate Output: Probability of distribution of coffee (0 to 1) MaxEnt model
  • 22. Bioclimatic variables for suitability modeling • Bio1 = Annual mean temperature • Bio2 = Mean diurnal range (Mean of monthly (max temp - min temp)) • Bio3 = Isothermality (Bio2/Bio7) (* 100) • Bio4 = Temperature seasonality (standard deviation *100) • Bio5 = Maximum temperature of warmest month • Bio6 = Minimum temperature of coldest month • Bio7 = Temperature Annual Range (Bio5 – Bi06) • Bio8 = Mean Temperature of Wettest Quarter • Bio9 = Mean Temperature of Driest Quarter • Bio10 = Mean Temperature of Warmest Quarter • Bio11 = Mean Temperature of Coldest Quarter • Bio12 = Annual Precipitation • Bio13 = Precipitation of Wettest Month • Bio14 = Precipitation of Driest Month • Bio15 = Precipitation Seasonality (Coefficient of Variation) • Bio16 = Precipitation of Wettest Quarter • Bio17 = Precipitation of Driest Quarter • Bio18 = Precipitation of Warmest Quarter • Bio19 = Precipitation of Coldest Quarter derived from monthly temperature & precipitation
  • 23. Coffee suitability - Maxent Results Nicaragua
  • 24. B Results Variable Adjusted R2 R2 due to variable % of total variability Present mean Change by 2050s Locations with decreasing suitability (n=89.8 % of all observations) BIO 14 – Precipitación del mes más seco 0.0817 0.0817 24.8 24.49 mm -3.27 mm BIO 04 – Estacionalidad de temperatura 0.1776 0.0959 29.1 0.83 0.166 BIO 12 – Precipitación anual 0.2057 0.0281 8.5 2462.35 mm -24.31 mm BIO 11 - Temperatura media del cuarto más frío 0.2633 0.0576 17.5 20.11 ºC 1.86 ºC BIO 19 - Precipitación del cuarto más frío 0.2993 0.0155 4.7 169.13 mm -7.08 mm BIO 05 - Temperatura máxima del mes más cálido 0.3198 0.0102 3.1 28.45 ºC 2.30 ºC BIO 13 - Precipitación del mes más húmedo 0.2838 0.0205 6.2 450.27 mm 10.72 mm Otros - - 6.2 Coffee suitability - Maxent Results Nicaragua
  • 25. B a Average of Q1 of GCMs b Average of GMSs c Average of Q3 of GCMs d Measure of agreement of models e standard deviation of GCMs b c e Uncertainty of model output (Maxent) using 19 GCMs SRES A2 – timeserie 2040 – 2069 (2050)
  • 26. Decision Support System for Agro technology Transfer (DSSAT) +
  • 27. • For 2 DSSAT-varieties (IB0006 ICTA-Ostua, IB0020 BAT1289 – “INTA Fuerte Sequia”, “INTA Rojo”, and “Tío Canela 75” originating from Nicaragua – “ICTA Ostua” and “ICTA Ligero” originating from Guatemala – “BAT 304” originating from Costa Rica – “SER 16”, SEN 56”, “NCB 226”, and “SXB 412” originating from CIAT, Colombia. • Sowing on: – Primera (Beginning of June) – Postrera (Beginning of September) • After recollecting data during 2011 results will be used in a post-project-analysis to calibrate 2 initial DSSAT varieties run it again for trial sites and find spatial and temporal analogues Accompanying field trials in 5 countries to calibrate DSSAT
  • 28. Planting date: Between 15th of April and 30th of June1 Variety 1: IB0006 ICTA-Ostua Variety 2: IB0020 BAT1289 Soil 1: IB00000005 (generic medium silty loam) Soil 2: IB00000008 (generic medium sandy loam) Fertilizer 1: 64 kg / ha 12-30-0 6 to 10 days after germination and 64 kg / ha Urea (46% N) at 22 to 25 days after germination. Fertilizer 2: 128 kg/ha 18-46-0 Fertilizer application on sowing and 64 kg/ha UREA at 22 to 30 days after germination. Weather data input: Current climate Average of 99 MarkSim daily outputs Future climate Ensemble of 19GCM & 99 MarkSim outputs for 2020 & 2050 Runs: 17,800 points x 3 climates x 99 MarkSim- samples x 8 trials DSSAT “Tortillas on the Roaster” in Central America
  • 29. Results: yield change for year 2020 (Primera) – 8 trials Trial 3 – high performance / high impact Variety 1: ICTA-Ostua Soil 1: generic medium silty loam Fertilizer 2: 128 kg/ha 18-46-0 Fertilizer application on sowing and 64 kg/ha UREA at 22 to 30 days after germination Trial 7 – medium high performance / less impact Variety 1: ICTA-Ostua Soil 2: generic medium sandy loam Fertilizer 2: 128 kg/ha 18-46-0 Fertilizer application on sowing and 64 kg/ha UREA at 22 to 30 days after germination
  • 30. Statistical negative and positive outliers of predicted yield change by 2020
  • 31. 31 Areas where the production systems of crops can be adapted Adaptation-Spots Focus on adaptation of production system Areas where crop is no longer an option Hot-Spots Focus on livelihood diversification New areas where crop production can be established Pressure-Spots Migration of agriculture – Risk of deforestation! Identifying Impact-Hot-Spots and select sites for socio-economic analysis
  • 32. 32 • Beans as most important income (sell 70% of harvest) • Climate variability (intense rain, drought), missing labor & credits, high input costs, … forces them to changes • Increasing livestock displace crops into hillside areas • Half of farmer rent their land • Distance to market is far • Mostly no road access in rainy season • They buy inputs/sell produce from/to farm-stores (they call them: Coyotes) Result: Sample-site 1 - Texistepeque (Las Mesas), Santa Ana ,El Salvador Message 2: Adaptation Strategies must be fine-tuned at each site! Las Mesas Altitude: 667 m (about 2188 feet) Hot-spot -141 kg/ha For 2020: • 35 mm less rain (current 1605mm) • mean temperature increase 1.1 C For 2050: • 73mm less rain ( -5%) • mean temperature increase 2.3 C • hottest day up to 35 C (+ 2.6 C) • coolest night up to 17.7 C (+ 1.8 C) Hot-spot
  • 33. 33 Message 3: There can be winners if they adapt quickly! Result: Sample-site 2 – Valle de Jamastran, Danlí, Honduras Adaptation-spot Jamastran Altitude: 783 m (about 2568 feet) Adaptation-spot - 115 kg/ha • Active communities with already advanced agronomic management of maize-bean crops • Favorable soil conditions and management • Long-term technical assistance / training • Irrigation schemes (e.g. 50 mz of 17 bean producers) • Diversification options (vegetables, livestock) • Market channels through processing industries • Advanced infrastructure (electricity, roads) • Need to optimize water use efficiency • Credit problems For 2020: • 41 mm less rain (current 1094 mm) • mean temperature increase 1.1 C For 2050: • 80 mm less rain ( -7%) • mean temperature increase 2.4 C • hottest day up to 34.2 C (+ 2.6 C) • coolest night up to 17 C (+ 2.1 C)
  • 34. Decision support system modelling (for benchmark sites) Agronomic management Expert & farmer survey Integrated crop-soil modeling 160 LDSF sample sites Baseline domains Impact 2030 A1b Experimental [n] cultivars [n] fertilizer application [n] seasons Application domains Analysis of biophysical systems and simulating crop yield in relation to management factors. Combine these models with field observations that allow adjustment of the models in the course of the growing season . Future 24 GCM A1B (IPCC) Current worldClim Validation with available station data Daily weather generator MarkSIM Weather station data (daily) Climate data yield soil management
  • 35. • Downscaling is inevitable. • Continuous improvements are being done • Strong focus on uncertainty analysis and improvement of baseline data • We need multiple approaches to improve the information base on climate change scenarios  Development of RCMs (multiple: PRECIS not enough)  Downscaling empirical, methods Hybrids  We tested different methodologies Conclusions climate data
  • 36. Conclusions crop models • Ecocrop, when there is a lack on crop information, for global or regional assessment • Maxent, perennial crops with presence only data (coordinates) available • DSSAT, only for few crops (beans, maize, …), high data input demand and calibrated field experiments are necessary • We need to communicate uncertainty of model predictions Empirical models Mechanistic models

Notes de l'éditeur

  1. Los escenarios de emisiones imponen condiciones para los modelos climáticos globales (basados en ciencias atmosféricas, química, física, biología, etc).Dividen el mundo el grillas y miran las relaciones entre factores que ocurren entre la atmósfera, los oceános, la superficie de la tierra. Por supuesto, hay cientos de procesos que salen de la comprensión de los modelos matemáticos así que estos modelos utilizan parametrizaciones para representar fenomenos incomprensibles. Son tan elaborados estos modelos que tienen que correrse en supercomputadoras. Entre más complejo sea el modelo, más factores tiene en cuenta y menos suposiciones usa. Se corre desde el pasado hasta el futuro
  2. Can you please take area per altitude line out? This is very important is shows that there is no more area available further up and that coffee will compete even more with protected areas. PES discussion.If you cannot, explain to what does it pertain: current or 2050? It simply shows the area available at each altitude current and future. Just area per altitude.
  3. The Decision Support System for Agrotechnology Transfer (DSSAT) is one of the most sophisticated crop simulation models currently available. Its advantages are the possibility to include specific information on weather, soils, plants, management and interactions of these factors.We ran DSSAT with available bean and maize variety calibration sets (2 fertilizer levels, 2 varieties, 2 soils, common smallholder conditions and management) to simulate current average yield and future expected yields. Results for current yields where ground-proofed through expert consultation throughout the region. In addition, field trials with recently introduced bean varieties with higher drought tolerance were conducted in order to obtain calibration data sets for more precise predictions.
  4. We ran the model for all the four countries and mapped the results (in this case the differences between current and future (2020) bean production) for Central America.As we can see there are areas where yields will decrease dramatically whereas others are improving their production potential. The already described changes in climate conditions and their interactions with other location specific conditions determine crop production. Heat and drought stress and high night temperatures are the main culprits for these results. This is broadly sustained by scientific evidence. Some general findings are:Beans : Temperatures > 28/18 C (day/night) decrease biomass production, seed-set, seed number and size (less pods per plant, lessseed per pod, lower seed weight) Elevated CO2 also decreased seed-set Elevated CO2 increased biomass, but benefits of elevated CO2 decreased with increasing temperaturesMaize: High temperature stress decreases pollination and seed set in maize, mainly caused by decreased pollen viability and stigma receptivity High temperature stress decreases seed-set and kernel numbers perplant. High temperature stress also affects negatively kernel quality and density (protein, enzymes) Reproductive stages (pollen development, flowering, early grain filling)are relatively more sensitive to drought stress, drought decreases kernel number and dry weights. Maize needs 50% of the water in the period 10 days before to 20 days after initial flowering. Even with enough water temperature stress affects pollen development. Drought stress decreases kernels numbers and kernel size Higher night temperatures means higher losses from respiration thus biomass and yield lossesFrom the DSSAT results we can now identify the different type of intervention areas in the region (next slide)
  5. As an example for a selected hot-spot location we presentTexistepeque / El Salvador where we find … (read the slide information)While we find several of these characteristics (e.g. coyotes as marketing channels) at other sites, each location shows also unique issues and combinations of factors and resources which make a specific fine-tuned adaptation strategies necessary. We pretend to build on several basic adaptation ideas which must be adapted to local conditions.
  6. Our second example shows that climate change might open up opportunities for people with advanced adaptation strategies and who will quickly apply these strategies.Although Jamastran will also be challenged from changes in climate conditions their degree of organization, available infrastructure and training may allow them to take advantage of the 1,000 mm of annual rainfall at this site. The already installed irrigation schemes and market intelligence open up opportunities (time windows) to produce bean and other products for markets when e.g. beans are not available (March-May). Also seed production in the dry season could be very lucrative. However, the intelligent use of water resources will be decisive.