Chapter 13 · Error growth in operational models
Overview
Everything so far has been measured by twin experiment: take a state, perturb it, integrate both copies, watch them separate. That method needs the truth.
A forecast centre does not have the truth. It has an analysis — itself a forecast, corrected by observations — whose own error is a substantial fraction of a short-range forecast’s, so verifying against it measures the forecast error plus the analysis error, correlated in ways that depend on the assimilation system. And there is no second Earth to perturb.
Lorenz (1982) answered this with an idea needing no truth at all. Two forecasts valid at the same time but started a day apart — a one-day and a two-day forecast, both verifying today — can be differenced from the archive alone. And their difference grows at the rate errors grow, because at the moment the older forecast reached yesterday it differed from yesterday’s analysis by roughly a one-day forecast error, and the two have been running together ever since.
The model
The trouble with a truth-free estimator is that you cannot check it against the truth. So this chapter builds a synthetic operational centre on Lorenz 96 where the truth is known and withheld: a cycling ensemble Kalman filter with six-hourly analyses, forecasts to thirty days from each of 600 consecutive analyses, and four observing networks from 40 observed sites down to 8. Then it runs Lorenz’s estimator — which sees only the forecasts — against the error curve computed from the truth.
chaoslib.errorgrowth.lagged_forecast_difference implements the estimator;
chaoslib.assimilate supplies the EnKF.
Three results
The estimator works, and not just for one fitted number. Across the three networks that have an exponential phase at all, the truth-free estimate recovers the true growth rate to within 2% at analysis errors of 0.5% and 2% of saturation, and 5% at 6%. More than that: plotting each curve’s local growth rate against its own amplitude, the two lie close together over the whole range — so the method recovers the rate at every error amplitude, including the amplitude-dependence chapter 9 established. The estimated curve sits below the true one, because it starts from a one-cycle forecast difference rather than the analysis error; that offset shifts the curve along the lead axis and leaves the rate alone, which is exactly why the method works.
It fails only where the archive offers nothing. With the analysis error at 45% of saturation there is no exponential phase, and the true rate is equally unmeasurable — a failure of the data, not the estimator.
The logarithmic return holds end to end. Thirteen times better analysis buys 7.0 days of lead time against 6.9 predicted from the measured growth rate — the same constant chapter 8 derived from and chapter 20 measured on a cycling system, obtained here a third way by building four observing networks and reading off the lead times.
The operational doubling time is not , and can be either side of it. Fitted at small error the rate is 1.91 per time unit — above , because a generic finite perturbation grows faster than the asymptotic rate over a finite window (chapter 16 measured optimal growth at 1.6–2.6× the Lyapunov estimate), and an analysis error is especially prone to it: the directions an observing network struggles with are not chosen at random relative to the ones that grow. Fitted at larger error the rate falls, per chapter 9. For this network the two effects give a doubling time of 1.86 days against the Lyapunov estimate’s 2.08. Which number to quote? None alone — an error-doubling time without a stated error amplitude is not a number.
What the method cannot see
Both forecasts in a lagged pair come from the same model, so anything systematically wrong with that model is common to both and cancels algebraically in the difference. The test for this adds a constant bias to an entire archive and asserts the estimator’s output is unchanged to round-off.
So the method measures growth of initial-condition error and is blind to model error by construction. A forecast system can be losing skill because its initial conditions are wrong or because its model is wrong, and this estimator reports only the first. Chapter 21 takes up model error, and chapter 22 the problem of verifying against observations that have errors of their own.
Exercises
Analytic. Show that if two forecasts valid at time were started one cycle apart, their difference at lead is the growth over of an initial difference equal to the one-cycle forecast error. Then explain why the resulting curve is offset from, but parallel to, the true error curve.
Computational. Reproduce the estimator’s ratio for all four networks at two fit windows. Explain why widening the window lowers both rates rather than degrading the agreement.
Exploratory. A model has a bias that grows with lead time. Predict what the lagged-forecast method reports, and say what additional information would be needed to detect the bias.
Further reading
- Lorenz, E. N. (1982). Atmospheric predictability experiments with a large numerical model. Tellus, 34, 505–513 — the lagged-forecast method.
- Simmons, A. J. and Hollingsworth, A. (2002). Some aspects of the improvement in skill of numerical weather prediction. QJRMS, 128, 647–677 [citation needed: confirm pages].
- Bengtsson, L. and Hodges, K. I. (2006). A note on atmospheric predictability [citation needed: journal and pages].
- Palmer, T. and Hagedorn, R., eds. (2006). Predictability of Weather and Climate, ch. 3 [citation needed: pages].