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The Analogues Methodology Julian Ramirez-Villegas
The method Jointly developed by the Walker Institute (University of Reading, UK) and the Decision and Policy Analysis program (DAPA) at CIAT Funded by CCAFS Theme 1: Adaptation to progressive climate change And collaborating with some other people in different institutions
Which questions can we answer? ,[object Object]
Where can I find a place that currently looks like how my site would be in the future? (BACKWARD)
Where can I find similar areas to my site currently or in the future? (NO-DIRECTION),[object Object]
Permit validation of computational models and trialing of new technologies and techniques
Learning from history
Ground climate change impacts and adaptation studies
Quantify the real effects of uncertainty in the process of adaptation,[object Object]
How do we calculate dissimilarity? The CCAFS measure: a modified version of the Euclidean distance m: time-step (e.g. month, day, quarter) v: number of variables V: Variable (i.e. temperature, rainfall, etc) W: Weight (any number or variable) f: reference scenario (e.g. future climate) p: target scenario (e.g. current climate) z: exponent (we normally assume 2) Lagging
How do we calculate dissimilarity? Accounting for lag Site A (southern) Site B (northern)
How do we calculate dissimilarity? The CCAFS measure: weights with other variables W: Weight value X: Variable value i: a given  time step j: a given variable
How do we calculate dissimilarity? As with the example data, m: month (from 1 to 12) f: reference value (e.g. future climate) p: target value (e.g. present climate) z: exponent (we normally assume 2) T: Temperature P: Precipitation DTR: Diurnal temperature range m-lag: month that produces a maximum match of climate parameters (precip, temp)
How do we calculate dissimilarity? Hallegatte et al. (2007): a rule based dissimilarity measure Relative difference between total values less than “a” Mean absolute relative differences between mean values for m steps less than “b” Mean absolute difference between total values for m steps less than “c” m: time-step (e.g. month, day, quarter) V: Variable (i.e. temperature, rainfall, etc) W: Weight (any number or variable) f: reference scenario (e.g. future climate) p: target scenario (e.g. current climate) a, b, c:  user defined parameters
Do our two measures agree? ,[object Object],[object Object],[object Object]
Analogues of what? ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]
Not so fast, though So we need to do it “through the eyes of the crop” Temperature and CO2 Avail. water and solar radiation Source: Bates, 2002 Source: Isdo et al., 1995 (sour orange trees)
Agricultural analogues ,[object Object],West et al. 2010, based on Monfreda et al. 2008
Agricultural analogues ,[object Object],Very similar high yield Very dissimilar and low yields
Important science questions ,[object Object]
If so, which variables do we need to use?
Rainfall + temperature?
Rainy days?
Days with extreme (very low, very high) temperatures?
Evapotranspiration?
Total thermal times?
Soils?

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The Analogues Methodology - Ramirez-Villegas

  • 1. The Analogues Methodology Julian Ramirez-Villegas
  • 2. The method Jointly developed by the Walker Institute (University of Reading, UK) and the Decision and Policy Analysis program (DAPA) at CIAT Funded by CCAFS Theme 1: Adaptation to progressive climate change And collaborating with some other people in different institutions
  • 3.
  • 4. Where can I find a place that currently looks like how my site would be in the future? (BACKWARD)
  • 5.
  • 6. Permit validation of computational models and trialing of new technologies and techniques
  • 8. Ground climate change impacts and adaptation studies
  • 9.
  • 10. How do we calculate dissimilarity? The CCAFS measure: a modified version of the Euclidean distance m: time-step (e.g. month, day, quarter) v: number of variables V: Variable (i.e. temperature, rainfall, etc) W: Weight (any number or variable) f: reference scenario (e.g. future climate) p: target scenario (e.g. current climate) z: exponent (we normally assume 2) Lagging
  • 11. How do we calculate dissimilarity? Accounting for lag Site A (southern) Site B (northern)
  • 12. How do we calculate dissimilarity? The CCAFS measure: weights with other variables W: Weight value X: Variable value i: a given time step j: a given variable
  • 13. How do we calculate dissimilarity? As with the example data, m: month (from 1 to 12) f: reference value (e.g. future climate) p: target value (e.g. present climate) z: exponent (we normally assume 2) T: Temperature P: Precipitation DTR: Diurnal temperature range m-lag: month that produces a maximum match of climate parameters (precip, temp)
  • 14. How do we calculate dissimilarity? Hallegatte et al. (2007): a rule based dissimilarity measure Relative difference between total values less than “a” Mean absolute relative differences between mean values for m steps less than “b” Mean absolute difference between total values for m steps less than “c” m: time-step (e.g. month, day, quarter) V: Variable (i.e. temperature, rainfall, etc) W: Weight (any number or variable) f: reference scenario (e.g. future climate) p: target scenario (e.g. current climate) a, b, c: user defined parameters
  • 15.
  • 16.
  • 17. Not so fast, though So we need to do it “through the eyes of the crop” Temperature and CO2 Avail. water and solar radiation Source: Bates, 2002 Source: Isdo et al., 1995 (sour orange trees)
  • 18.
  • 19.
  • 20.
  • 21. If so, which variables do we need to use?
  • 24. Days with extreme (very low, very high) temperatures?
  • 30.
  • 31.
  • 32. How to calculate climate analogues online and via R
  • 33. The different sensitivities of this method (variables, weights, direction)
  • 34.
  • 35. A couple of clarifications… Similarity between EcoCrop response and other models