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Carlos Navarro
J. Tarapues, J. Ramirez, A. Jarvis
Major global dataset:
CCAFS-Climate
Concepts Homogenization
• General Circulation Model (GCM): is a type of climate
model. It employs a mathematical model of the general
circulation of a planetary atmosphere or ocean. These
models are the basis for model predictions of future
climate, such as are discussed by the IPCC.
• Downscaling: is a general concept that embraces various
methods for increasing the spatial resolution and reduce
some of the biases in order to improve the usability of
climate scenarios.
• Bias correction: correct the climate input data provided
by GCM for systematic statistical deviations from
observational data. They generally adjust the long-term
mean by adding the average difference between the
simulated and observed data over the historical period to
the simulated data, or by applying an associated
multiplicative correction factor.
Climate and Agriculture
Needs
Limitations
• Multiple variables
• Very high spatial
resolution
• Mid-high temporal (i.e.
monthly, daily) resolution
• Accurate weather
forecasts and climate
projections
• High certainty. Both for
present and future
–T°
• Max,
• Min,
• Mean
–Prec
–HR
– Radiation
– Wind
– …….
Lessimportance
Morecertainty
Climate and Agriculture
Agriculture, a niche business
Global scale 
Regional or local scale 
Resolutions
• Horizontal resolution 100 to
300 km
GCMs are the only way
we can predict the future
climate
GCM “Global Climate Model”
Problems
Needs
Options
• Statistical or dynamical
downscaling methods.
• Bias correction
methods.• Correct biases
• Provide high
resolution and
contextualized data
• Systematic errors or biases.
• Low resolution (> 50 Km).
• Incomplete knowledge of
climate system processes.
• High deviations from
observational data.
Why Do We Need Downscaling?
Hawkins, 2012
GCM Biases and Calibration
http://ccafs-climate.org
Ramírez-Villegas and Challinor, 2012
AI GCM: GCM data “as is”, SD GCM: statistically
downscaled GCM, PS GCM: pattern scaled GCM,
WG GCM: GCM data through a weather
generator, SC Variables: systematic changes in
target key variables, Unclear: not specified clearly
in study, ARPEGE: the ARPEGE Atmospheric GCM
Downcaling by serveral methods in CCAFS-
Climate
Sessions
126,768
Users
66,682
Page Views
466,120
Pages/Session
3.68
Avg. Session Duration
00:04:44
Bounce Rate
42.11%
Significant impact by
putting climate change
information into the hands
of non-climate scientists
and next users which
represent up to 19% of all
CCAFS-Climate users.
> 400 Publications
CORDEX Dynamical Downscaled Data
Undefined periods
Prec, Tmax, Tmin, Bioclim + otrhers
0.44deg (~50km)
At least 2 CORDEX Domains
2014
ETA Dynamical Downscaled Data
4 GCM - 2 SCENARIOS,
4 future periods.
0.33deg (~40km)
South America
4 RCP
106 GCM (about 25 models per RCP)
4 future periods
5 climatological variables
4 spatial resolutions (the highest at 1 Km2)
Full set of CMIP5 Delta Method
Downscaled Data
CMIP5 Raw and Processed Daily Data with several bias-correction
Methodologies (Online processing)
2015-2016
DSSAT (.wtg)
APSIM (json)
Others (ascii)
2030’s, 2050’s, 2070’s, 2080’s
Prec, Tmax, Tmin, Rsds
Raw Resolution
Extractions online in
formats of interest to
Crop Modelers
We are focused now in
increase its use amongst
crop modelers
http://ccafs-climate.org/data_bias_corrected/
http://www.ccafs-climate.org/weather_stations
Climate Wizard
integration
• A major barrier preventing informed climate-change adaptation planning is the
difficulty accessing, analyzing, and interpreting climate-change information.
http://climatewizard.ciat.cgiar.org/
Applied climate change analysis
• Provides non-climate specialists with simple
analyses and innovative graphical depictions
for conveying.
• Provides both the data for impacts research, as
well as the basic information that is needed to
understand the IPCC climate projections within
specific geographic areas throughout the
world. Provides projections for policy and
practice.
• It can get relatively complicated (such as when
you visualize changing probabilities of extreme
events) or it can be simple such as looking at
maximum temperatures during a month of
interest
WOCAT Integration
The World Overview of Conservation
Approaches and Technologies
API development:
• Developer for
WOCAT
Sustainable Land
Management
Database
• API to query
climate change
projections from
ClimateWizard
GCMs
Effective
adaptation
options
MarkSim
DSSAT
Statistical Downscaling
Dynamical downscaling:
Regional Climate Model
EcoCrop
Statistical
Downscaling
MaxEnt
Based on niches
Probability
Environmental gradient
Based on process
We use calibrated GCM to quantify the impacts
and adaptation options through crops models
Gourdji et al. (in prep.)
Percent change in yields by 2030s and RCP4.5
Using crop models to look at crop yields
under future climate
Vallejo and Ramirez-Villegas, BID Report (2016)
Rainfed
agriculture
vulnerability
hotspots
… and to identify vulnerability hotspots
So take a look…Conservation plans, niche
models, crop models, and
biodiversity evaluation require
high resolution inputs.
Downscaling produces precise
tools that allow local rather
than regional or global
predictions of climatic
changes.
CCAFS-Climate is a web service
to query Downscaled data, Bias
Corrected data and weather
information for a broad of user,
not only scientist.
Conclusions
Carlos Navarro-Racines
c.e.navarro@cgiar.org

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Navarro-Racines_C Major global dataset: CCAFS-Climate

  • 1. Carlos Navarro J. Tarapues, J. Ramirez, A. Jarvis Major global dataset: CCAFS-Climate
  • 2. Concepts Homogenization • General Circulation Model (GCM): is a type of climate model. It employs a mathematical model of the general circulation of a planetary atmosphere or ocean. These models are the basis for model predictions of future climate, such as are discussed by the IPCC. • Downscaling: is a general concept that embraces various methods for increasing the spatial resolution and reduce some of the biases in order to improve the usability of climate scenarios. • Bias correction: correct the climate input data provided by GCM for systematic statistical deviations from observational data. They generally adjust the long-term mean by adding the average difference between the simulated and observed data over the historical period to the simulated data, or by applying an associated multiplicative correction factor.
  • 4. • Multiple variables • Very high spatial resolution • Mid-high temporal (i.e. monthly, daily) resolution • Accurate weather forecasts and climate projections • High certainty. Both for present and future –T° • Max, • Min, • Mean –Prec –HR – Radiation – Wind – ……. Lessimportance Morecertainty Climate and Agriculture Agriculture, a niche business
  • 5. Global scale  Regional or local scale  Resolutions • Horizontal resolution 100 to 300 km GCMs are the only way we can predict the future climate GCM “Global Climate Model”
  • 6. Problems Needs Options • Statistical or dynamical downscaling methods. • Bias correction methods.• Correct biases • Provide high resolution and contextualized data • Systematic errors or biases. • Low resolution (> 50 Km). • Incomplete knowledge of climate system processes. • High deviations from observational data. Why Do We Need Downscaling?
  • 7. Hawkins, 2012 GCM Biases and Calibration
  • 9. Ramírez-Villegas and Challinor, 2012 AI GCM: GCM data “as is”, SD GCM: statistically downscaled GCM, PS GCM: pattern scaled GCM, WG GCM: GCM data through a weather generator, SC Variables: systematic changes in target key variables, Unclear: not specified clearly in study, ARPEGE: the ARPEGE Atmospheric GCM Downcaling by serveral methods in CCAFS- Climate
  • 11. Significant impact by putting climate change information into the hands of non-climate scientists and next users which represent up to 19% of all CCAFS-Climate users. > 400 Publications
  • 12. CORDEX Dynamical Downscaled Data Undefined periods Prec, Tmax, Tmin, Bioclim + otrhers 0.44deg (~50km) At least 2 CORDEX Domains 2014 ETA Dynamical Downscaled Data 4 GCM - 2 SCENARIOS, 4 future periods. 0.33deg (~40km) South America 4 RCP 106 GCM (about 25 models per RCP) 4 future periods 5 climatological variables 4 spatial resolutions (the highest at 1 Km2) Full set of CMIP5 Delta Method Downscaled Data CMIP5 Raw and Processed Daily Data with several bias-correction Methodologies (Online processing) 2015-2016 DSSAT (.wtg) APSIM (json) Others (ascii) 2030’s, 2050’s, 2070’s, 2080’s Prec, Tmax, Tmin, Rsds Raw Resolution Extractions online in formats of interest to Crop Modelers We are focused now in increase its use amongst crop modelers
  • 15. Climate Wizard integration • A major barrier preventing informed climate-change adaptation planning is the difficulty accessing, analyzing, and interpreting climate-change information. http://climatewizard.ciat.cgiar.org/ Applied climate change analysis • Provides non-climate specialists with simple analyses and innovative graphical depictions for conveying. • Provides both the data for impacts research, as well as the basic information that is needed to understand the IPCC climate projections within specific geographic areas throughout the world. Provides projections for policy and practice. • It can get relatively complicated (such as when you visualize changing probabilities of extreme events) or it can be simple such as looking at maximum temperatures during a month of interest
  • 16. WOCAT Integration The World Overview of Conservation Approaches and Technologies API development: • Developer for WOCAT Sustainable Land Management Database • API to query climate change projections from ClimateWizard
  • 17. GCMs Effective adaptation options MarkSim DSSAT Statistical Downscaling Dynamical downscaling: Regional Climate Model EcoCrop Statistical Downscaling MaxEnt Based on niches Probability Environmental gradient Based on process We use calibrated GCM to quantify the impacts and adaptation options through crops models
  • 18. Gourdji et al. (in prep.) Percent change in yields by 2030s and RCP4.5 Using crop models to look at crop yields under future climate
  • 19. Vallejo and Ramirez-Villegas, BID Report (2016) Rainfed agriculture vulnerability hotspots … and to identify vulnerability hotspots
  • 20. So take a look…Conservation plans, niche models, crop models, and biodiversity evaluation require high resolution inputs. Downscaling produces precise tools that allow local rather than regional or global predictions of climatic changes. CCAFS-Climate is a web service to query Downscaled data, Bias Corrected data and weather information for a broad of user, not only scientist. Conclusions

Hinweis der Redaktion

  1. Necesidades 1) Cualquier agroecosistema responde a: Factores antropogénicos, Bioticos, Abióticos 2) Cálculos de vulnerabilidad Desarrollar modelos → Conocer incertidumbres → Planes de acción → Generación de políticas   Limitaciones 1) Modelos todavía no pueden representar cientos de procesos de forma adecuada 2) Resoluciones de modelos inadecuadas: Se requieren modelos con escalas finas. 3) Incertidumbres: futuras emisiones f(suposiciones concentraciones, población, desarrollo económico, tecnológico)
  2. Agriculture is a niche based activity, and then we need climate data to characterize the niche. In relation to climate and agriculture, agriculture demands to multiple variables like precipitation, temperature, wind speed, soil moisture, solar radiation, relative humid, among many others. Agriculture demands very high spatial resolution, maybe 1km, ninty meters.. Also, agriculture needs a Mid-high temporal resolution. We need at least montly climate data and for some application we need daily data for example mechanistic crops models .. Both for present and future For adaptation plans we need high certainty.. Mainly for precipitation
  3. Estos modelos pueden llegar a ser tan complejos que pueden expandirse verticalmente a muchos niveles, sin embargo las resoluciones espaciales de sus salidas no son las más adecuadas. Fenómenos escala local : Especialmente en regiones con orografía compleja, suelo hetereogéneo, línea costas.
  4. Características del clima no observables en los GCMs Temperaturas frias de los alpes Amplio rango de temperaturas Corrección Bias Muchos cultivos son sensibles a umbrales de T
  5. Grado de cobertura diff segun modelo. Y resultados tambien yield o suitability. Tambien difieren en escala espacio-temporal a la que se usan.
  6. We see crop areas which are impacted positively or negatively by climate change. We use DSSAT model. Grains like Maize (<) But for example rice (>)
  7. We use in general change in climate to identify hotpots but also we use socio-economic variables to project change in yields. Per capita income change. We see at regional level wich productive areas will be greater affected by climate change and also change in population dynamics.
  8. Linkear Cambios en adaptabilidad Testimonials from farmers in the area of interest Descripciones de los sitios Will be linked to Agtrials and the Analogue tool.