Title: Quantify prediction uncertainty(Book, p. 174-189)
1Quantify 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
2Quantify 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).
3Individual 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
4Exercise 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.
5Calculating linear intervals with
UCODE_2005. From Poeter , 2005, p. 158)
6Linear 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
7Figure 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
8Results of Exercise 8.2a(continued)Linear
Confidence Intervals for Question 5 What is the
prediction uncertainty?
Figure 8.16, p. 211
9Nonlinear 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.
10Calculating nonlinear intervals with
UCODE_2005. Modified from Poeter , 2005, p. 193)
11Nonlinear 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
12Figure 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
13Linear Individual
Linear Simultaneous (Scheffe dNP)
Figure 8.15a, p. 210
Figure 8.15, p. 210
Nonlinear Simultaneous (Scheffe dNP)
Nonlinear Individual
14Our 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
15Monte 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)
16Can 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.
17Can 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.