Quantify prediction uncertainty(Book, p. 174-189) - PowerPoint PPT Presentation

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Quantify prediction uncertainty(Book, p. 174-189)

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Title: Quantify prediction uncertainty(Book, p. 174-189)


1
Quantify prediction uncertainty(Book, p. 174-189)
  • Prediction standard deviations (Book, p. 180)
  • A measure of prediction uncertainty
  • Calculated by translating parameter uncertainty
    through to the predictions
  • Activate all parameters when calculating !!!
  • Calculate parameter var-cov matrix with all
    parameters
  • Calculate prediction sensitivities for all
    parameters

2
Quantify prediction uncertainty
  • Linear confidence and prediction intervals (p.
    176-177)
  • Intervals can be individual or simultaneous
  • Form confidence interval prediction
    interval
  • Prediction intervals account for measurement
    error. Use to compare simulated results to field
    measurements.
  • a is the significance level, c(a) is the critical
    value and is different for different types of
    intervals (Table 8.1, p. 176).

3
Individual vs. Simultaneous Intervals
  • Individual linear intervals
  • Defined as an interval that has a specified
    probability of containing the true predicted
    value.
  • Exact for correct, linear models with normally
    distributed residuals.
  • The more these requirements are violated, the
    less accurate the intervals become.
  • Simultaneous linear intervals
  • On two or more predictions, each has a specified
    probability of containing the true value.
  • Always linear intervals, because of greater
    difficulty in defining intervals that
    simultaneously include true values of two or more
    predictions. Largest intervals are for case where
    of predictions of parameters
  • Common types Bonferoni Sheffé

4
Exercise 8.2a Calculate linear confidence
intervals on predicted advective transport
  • Linear confidence intervals can be computed in
    UCODE_2005 using program Linear_Uncertainty.exe.
  • Linear_Uncertainty uses V(b) from the regression
    run output, along with information from an extra
    ucode run with the prediction conditions (for
    computing prediction sensitivities) to calculate
    prediction standard deviations.
  • Then it calculates the different types of
    individual and simultaneous intervals using the
    appropriate statistics.

5
Calculating linear intervals with
UCODE_2005. From Poeter , 2005, p. 158)
6
Linear Intervals
  • Do Exercise 8.2a (p. 208-209) and the Problem,
    including answering Question 5 What is the
    uncertainty in the predictions?
  • Correction to book p. 208, second line from the
    bottom, should read Answer Question 5

7
Figure 8.15a, p. 210
Linear Individual
Results of Exercise 8.2aLinear Confidence
Intervals for Question 5 What is the prediction
uncertainty?
Linear Simultaneous (Scheffe dNP)
Figure 8.15b, p. 210
8
Results of Exercise 8.2a(continued)Linear
Confidence Intervals for Question 5 What is the
prediction uncertainty?
Figure 8.16, p. 211
9
Nonlinear Intervals
Method involves finding the minimum and maximum
predicted value on a confidence region for the
parameters, which is defined as (book, p.
178) S(b) ? S(b) (s2 x crit) a
critcritical value
Maximum prediction
Minimum prediction
Developed by Vecchia and Cooley (1987, WRR) Each
limit of each interval requires a regression run
that is often more difficult than the regression
runs used for calibration.
10
Calculating nonlinear intervals with
UCODE_2005. Modified from Poeter , 2005, p. 193)
11
Nonlinear Intervals
  • Do exercise 8.2b
  • Computer instructions the input files are
    provided for you in initial\ex8\ucode-opr-ppr-runs
    \ex8.2b directory, as noted in the computer
    instructions.
  • The nonlinear intervals are in ex8.2b._intconf

12
Figure 8.15c, p. 210
Nonlinear Individual
Results of Exercise 8.2bNonlinear Confidence
Intervals for Question 5 What is the prediction
uncertainty?Do the Problem on p. 212
Nonlinear Simultaneous (Scheffe dNP)
Figure 8.15d, p. 210
13
Linear Individual
Linear Simultaneous (Scheffe dNP)
Figure 8.15a, p. 210
Figure 8.15, p. 210
Nonlinear Simultaneous (Scheffe dNP)
Nonlinear Individual
14
Our Final Analysis and the County Decision
  • Our Analysis
  • Though it looks likely that the particle goes to
    the well, results are not conclusive.
  • Consider using parameter values for which the
    particle goes to the river in an
    advective-dispersive model to analyze
    concentrations at the well. If concentrations
    high, results become more conclusive.
  • County decision
  • No additional modeling right now
  • Wait for the new data and use it to recalibrate

15
Monte Carlo Analysis (Book, p. 185-189)
  • Change some aspect of model input, run model,
    evaluate selected changes in model results.
  • Can change parameter values, definition of
    hydrogeology, etc.
  • When changing parameter values, can generate new
    sets from V(b) if model was calibrated by
    regression. For changing hydrogeology, a common
    geostatistical approach is simulation, which
    uses kriging as part of the method.
  • Can just do forward simulations, or can involve
    inverse modeling as well.
  • Commonly need to do numerous model runs to obtain
    enough data to make supportable conclusions.
    This is now often feasible, with the level of
    computational power in PCs.
  • Results commonly displayed as histograms showing
    distribution of model output values can also
    calculate statistics from the results, such as
    means and variances.
  • Suggestion only use sets of generated parameter
    values that produce a reasonable fit to the
    calibration data (Beven)

16
Can confidence intervals replace traditional
sensitivity analysis? (p. 184-185)
  • Traditional sensitivity analysis
  • quantify uncertainty in the calibrated model
    caused by uncertainty in the estimated parameter
    values
  • change hydraulic conductivity, storage, recharge
    and boundary conditions systematically within
    previously established plausible range
  • Weaknesses of traditional method
  • Plausible range does not reflect significant
    information provided through model calibration.
    Results exaggerate uncertainty.
  • Suggested method to account for parameter
    correlation exacerbates this exaggeration.

17
Can confidence intervals replace traditional
sensitivity analysis?
  • Weaknesses of both methods
  • Only consider uncertainty in the parameter
    values.
  • Uncertainty in model construction generally
    neglected entirely
  • Advantages of confidence intervals
  • Account for information provided through the
    modeling process.
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