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Presenting objective and subjective uncertainty
  information for spatial system-based models.

                                    Kim Lowell
Presenting Objective and Subjective
 Uncertainty Information for Spatial
              System-based Models
                  Kim Lowell1,2, Brendan Christy1, Greg Day1
                                           1Department of Primary Industries
                    2CRC   for Spatial Information, University of Melbourne
The Rise of Models

 Land management increasingly holistic
     Multiple outcome questions
     Systems-science

 More reliance on models for Public Policy

 Increased model use demands increased model
  meta-data
     Uncertainty especially
Project Context
 Victorian Government Water White Paper
     Action 2.20 – Water and forest plantations
     Modelling to identify best” locations
“Spatial Viewer”

 Increased
  flexibility for
  non-
  technical
  model users
Spatial Viewer Summary
 Land-use change among:
     Pasture, Crop, Forest

 Impact on eight factors:
       Aquifer recharge
       Evapotranspiration (ET)
       Flow to stream
       Plant carbon
       Erosion
       In-stream phosphorous
       In-stream nitrogen
       In-stream salt load
       Depth-to-water table
CAT Model Background
 Catchment Analysis Tool (CAT)
 Underpinning hydrological model
 Linked single-purpose
  landscape models
     Erosion
     Tree growth
     Etc.
CAT Calibration
Calibrated for each catchment
Data
     Bore holes (water depth)   80000


     Climate (rainfall)         70000
                                 60000
                                 50000

     Streamflow (outflow)       40000
                                 30000
                                                                                                                           Realm_Strm
                                                                                                                          Modelled_Strm

                                 20000
                                 10000
                                    0


 Method



                                         Jul-74

                                                  Jul-77

                                                           Jul-80

                                                                    Jul-83

                                                                             Jul-86

                                                                                      Jul-89

                                                                                               Jul-92

                                                                                                        Jul-95

                                                                                                                 Jul-98
     Numerical optimisation
     Expert knowledge
     Voodoo
Implications for Uncertainty

 Objective estimation not possible for all
  parameters

 Truly independent validation not possible

 Model complexity limits numerical evaluation
     Size of error
     Form of error distribution
Policy Makers . . . .
 “I understand all that, but all I want to know is if the
  model estimates are „good‟.”
Solution
 Spatial and statistical uncertainty information

 Statistical on stream gauges
     Coefficient of efficiency:
       – CE = 1 - Σ(Oi - Pi)2/Σ(Oi – OBar)2         (1)
       – where Oi and Pi are Observed and Predicted
       – OBar is the average observed value over entire
         period
Interpretation of CE
 >0.6 “Satisfactory”; > 0.8 “Good”
                                                                    B a s e flo w (C o r a n g a m ite )                                                                                Q u ic k flo w (C o r a n g a m ite )
        C o e ffic ie n t o f E ffic ie n c y




                                                                                                                           C o e ffic ie n t o f E ffic ie n c y
                                                  1
                                                                                                                                                                              1


                                                0. 8
                                                                                                                                                                             0.8


                                                0. 6
                                                                                                                                                                             0.6


                                                0. 4                                                                                                                         0.4


                                                0. 2                                                                                                                         0.2


                                                  0                                                                                                                           0
                                                       0    5             10         15        20          25    30   35                                                            0   5         10         15          20       25    30
                                                                               S tre a m G a u g e ID                                                                                             S tr e a m G a u g e ID



                                                           In -s tr e a m S a lt (C o r a n g a m ite )                                                                                 S tr e a m flo w (C o r a n g a m ite )




                                                                                                                                     C o e ffic ie n t o f E ffic ie n c y
     C o e ffic ie n t o f E ffic ie n c y




                                                  1                                                                                                                            1



                                                0.8                                                                                                                          0. 8



                                                0.6                                                                                                                          0. 6



                                                0.4                                                                                                                          0. 4



                                                0.2                                                                                                                          0. 2



                                                  0                                                                                                                            0
                                                       0        5              10         15         20         25    30                                                            0    5         10         15          20       25    30

                                                                               S tr e a m G a u g e ID                                                                                             S tr e a m G a u g e ID
Spatial Uncertainty
 Reflects the calibration data and method

 For example….
     Stream gauges +         Limits to numerical
      flow directions            evaluation
Uncertainty Surfaces
For Users of Model Outputs




                                                   S tr e a m flo w (C o r a n g a m ite )
C o e ffic ie n t o f E ffic ie n c y




                                          1



                                        0. 8



                                        0. 6



                                        0. 4



                                        0. 2



                                          0
                                               0    5         10         15          20      25   30

                                                              S tr e a m G a u g e ID
Conclusions

 Model uncertainty can be communicated
  without hard statistics.

 Combining numerical/objective and
  qualitative/subjective information is useful.

 Uncertainty representation must reflect model
  fundamentals.
The Environment
    Institute

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Presenting objective and subjective uncertainty information for spatial system-based models

  • 1. Presenting objective and subjective uncertainty information for spatial system-based models. Kim Lowell
  • 2. Presenting Objective and Subjective Uncertainty Information for Spatial System-based Models Kim Lowell1,2, Brendan Christy1, Greg Day1 1Department of Primary Industries 2CRC for Spatial Information, University of Melbourne
  • 3. The Rise of Models  Land management increasingly holistic  Multiple outcome questions  Systems-science  More reliance on models for Public Policy  Increased model use demands increased model meta-data  Uncertainty especially
  • 4. Project Context  Victorian Government Water White Paper  Action 2.20 – Water and forest plantations  Modelling to identify best” locations
  • 5. “Spatial Viewer”  Increased flexibility for non- technical model users
  • 6. Spatial Viewer Summary  Land-use change among:  Pasture, Crop, Forest  Impact on eight factors:  Aquifer recharge  Evapotranspiration (ET)  Flow to stream  Plant carbon  Erosion  In-stream phosphorous  In-stream nitrogen  In-stream salt load  Depth-to-water table
  • 7. CAT Model Background  Catchment Analysis Tool (CAT)  Underpinning hydrological model  Linked single-purpose landscape models  Erosion  Tree growth  Etc.
  • 8. CAT Calibration Calibrated for each catchment Data  Bore holes (water depth) 80000  Climate (rainfall) 70000 60000 50000  Streamflow (outflow) 40000 30000 Realm_Strm Modelled_Strm 20000 10000 0  Method Jul-74 Jul-77 Jul-80 Jul-83 Jul-86 Jul-89 Jul-92 Jul-95 Jul-98  Numerical optimisation  Expert knowledge  Voodoo
  • 9. Implications for Uncertainty  Objective estimation not possible for all parameters  Truly independent validation not possible  Model complexity limits numerical evaluation  Size of error  Form of error distribution
  • 10. Policy Makers . . . .  “I understand all that, but all I want to know is if the model estimates are „good‟.”
  • 11. Solution  Spatial and statistical uncertainty information  Statistical on stream gauges  Coefficient of efficiency: – CE = 1 - Σ(Oi - Pi)2/Σ(Oi – OBar)2 (1) – where Oi and Pi are Observed and Predicted – OBar is the average observed value over entire period
  • 12. Interpretation of CE  >0.6 “Satisfactory”; > 0.8 “Good” B a s e flo w (C o r a n g a m ite ) Q u ic k flo w (C o r a n g a m ite ) C o e ffic ie n t o f E ffic ie n c y C o e ffic ie n t o f E ffic ie n c y 1 1 0. 8 0.8 0. 6 0.6 0. 4 0.4 0. 2 0.2 0 0 0 5 10 15 20 25 30 35 0 5 10 15 20 25 30 S tre a m G a u g e ID S tr e a m G a u g e ID In -s tr e a m S a lt (C o r a n g a m ite ) S tr e a m flo w (C o r a n g a m ite ) C o e ffic ie n t o f E ffic ie n c y C o e ffic ie n t o f E ffic ie n c y 1 1 0.8 0. 8 0.6 0. 6 0.4 0. 4 0.2 0. 2 0 0 0 5 10 15 20 25 30 0 5 10 15 20 25 30 S tr e a m G a u g e ID S tr e a m G a u g e ID
  • 13. Spatial Uncertainty  Reflects the calibration data and method  For example…. Stream gauges + Limits to numerical flow directions evaluation
  • 15. For Users of Model Outputs S tr e a m flo w (C o r a n g a m ite ) C o e ffic ie n t o f E ffic ie n c y 1 0. 8 0. 6 0. 4 0. 2 0 0 5 10 15 20 25 30 S tr e a m G a u g e ID
  • 16. Conclusions  Model uncertainty can be communicated without hard statistics.  Combining numerical/objective and qualitative/subjective information is useful.  Uncertainty representation must reflect model fundamentals.
  • 17. The Environment Institute