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The impenetrable hedge: some thoughts on propriety, equitability and consistency

The impenetrable hedge: some thoughts on propriety, equitability and consistency. Forecast verification Hedging Propriety Equitability Consistency. Ian Jolliffe. Forecast verification. Forecasts of weather and climate are made at all timescales.

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The impenetrable hedge: some thoughts on propriety, equitability and consistency

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  1. The impenetrable hedge: some thoughts on propriety, equitability and consistency • Forecast verification • Hedging • Propriety • Equitability • Consistency Ian Jolliffe Exeter, February 2008

  2. Forecast verification • Forecasts of weather and climate are made at all timescales. • It is desirable to verify/validate/assess forecasts • Science: A look back at the accuracy of forecasts is necessary to determine whether current forecasting methods should be continued, abandoned or modified. • Users: Decisions are based on past data but also on forecasts of data not yet observed.

  3. Verification measures • In a measures-oriented approach toforecast verification, the value of one or more measure that quantifies desirable properties of a set of forecasts is calculated. • Often a variety of measures or scores is available for a set of forecasts. To choose between them, desirable properties of the measures themselves have been defined. This is called metaverification. • Such criteria include propriety, consistency and equitability, all of which relate to the avoidance of hedging.

  4. Hedging • Hedging has a variety of definitions, but is commonly taken in everyday use to mean ‘placing bets on the opposite side in order to cut losses or guarantee a minimum amount of winnings’. In other words a forecast allows more than one (conflicting) possibility. • The term is fairly well-known in meteorology, though not very often used in print. When it is, it is taken to mean that it occurs (Murphy, 1978) ‘whenever a forecaster’s judgement and forecast differ’.

  5. To hedge or not to hedge • ‘A meteorologist who prepares probability forecasts should not “hedge,” i.e. the meteorologist’s probabilities should express his true beliefs’. • ‘A meteorologist whose forecasts are evaluated with a particular scoring system can, and should, be expected to “hedge” to obtain the best possible score.’ • Both quotations express plausible positions. Both are from Murphy & Epstein (1967), the latter deriving from a panel discussion reported in BAMS (1952).

  6. Why hedge? • Hedging is used to make some sort of gain over what can be achieved without hedging. • In everyday usage the gain is financial. • In meteorology the gain is a better value or expected value of some score used to assess/verify forecasts. Hence hedging is ‘playing the score’. • To make both quotations compatible we can restrict ourselves to using scores for which hedging is impossible – we need proper, or consistent, or perhaps equitable, scores. • Caveat: If missing an extreme event is far more costly than a ‘false alarm’, hedging by over-forecasting is actually desirable. This is because the concept of value comes into play.

  7. Finley’s tornados • Finley’s classic tornado forecasts: • Consider the measure Proportion Correct (PC) = (a+d)/n = 2708/2803 = 0.966. • The naïve strategy of always forecasting ‘no tornado’ does better (2752/2803 = 0.981), so PC can be hedged.

  8. Value of Tornado Forecasts • If a wrong forecast of any sort costs $1K, then the cost of the forecasting system is $95K, but the naive system costs only $51K – so the forecast system should not be used. • However, if a false alarm costs $1K, but a tornado missed costs $10K, then the system costs $302K, but naivety costs $510K. So the forecasting system saves $208K compared to naivety. • … not to mention lives. • Following Finley’s article, Peirce (1884) not only devised an equitable score, but looked at ‘utility’, associating a ‘profit’ with hits and ‘loss’ with false alarms.

  9. Propriety (proper scores) • Next they should be taught about equitability and consistency.

  10. Propriety II • For probability forecasts, a (strictly) proper scoring system is one for which the forecaster obtains the best possible expected score by forecasting his/her true beliefs (and only by doing so) – Murphy & Epstein, 1967. • It is not necessary to invoke a ‘true belief’ to argue for propriety – Broeker and Smith, 2007. • The Brier score is the best known proper score – there are others (logarithmic, spherical), also plenty of theory and discussion. Equally, many scores (e.g. linear) are not proper.

  11. Propriety is irrelevant for deterministic forecasts Either • The forecaster’s true belief is probabilistic. Or • The forecast is certain his/her (deterministic) forecast is correct, so the best possible value of the score will be achieved for any score, and there is no incentive to hedge.

  12. Equitability • ‘All’ unskilled forecasts should have the same expected score. • Not so obviously related to hedging as propriety. • But if a score is not equitable, it can be hedged in the sense that a forecaster who knows (s)he has little skill may do better using an unskilled forecast with a better expected score.

  13. Equitability – what is an ‘unskilled’ forecast? • Choosing a forecast by some completely random mechanism. • Always making the same forecast (but what if that forecast is ‘climatology’?) • Forecasting persistence?? Most definitions include 1 & 2, but not 3.

  14. Propriety and equitability No scoring system for probability forecasts can be both proper and equitable. Given the choice, which would you prefer? • Propriety or equitability?

  15. Equitability and probability forecasts • Not only is equitability incompatible with propriety, but it is rather difficult to achieve equitability at all for probability forecasts. • Any score is a function S(d) of the difference d=f-o, where f is forecast probability and o the corresponding observation, which is always 0 or 1. • If S(d) is required to be symmetric [S(d)=S(-d)], then equitability is impossible unless • S(p) = S(1-p) for all p between 0 and 1 or • The base rate/climatology θ is equal to 0.5. • The second of these conditions is very restrictive and the first makes no sense.

  16. Equitability and probability forecasts II • What about allowing non-symmetry of S(d)? It is then relatively easy to get an equitable score. • Arbitrarily set S(0) = 0, S(1) =1 (other ‘anchor points’ give qualitatively similar conclusions). • The nature of the asymmetry is determined by the base rate θ. • For θ = 1/3, S(1) = 1 and S(-1) = 2. • For θ = 0.1, S(1) = 1 and S(-1) = 9. • It is plausible that a highly asymmetric score might be needed when ‘value’ is taken into account; much less so that the asymmetry is determined solely by base rate … • But perhaps penalising wrong forecasts a long way from base rate less than wrong forecasts close to base rate has some merit??

  17. Consistency • For deterministic forecasts ‘consistency’ takes the place of ‘propriety’. • Like ‘hedging’ the meaning is slightly different from everyday usage. • There are ‘consistent’ forecasts – those that correspond with the forecaster’s judgments i.e. the forecaster does not hedge (Murphy, 1993). • There are also ‘consistent’ performance measures (scores) …

  18. Consistent scores • For the definition of consistency given by Murphy & Daan (1985) we need to assume that any forecaster really has a probability distribution for the variable to be forecast and that a rule or directive determines the deterministic forecast to be made, given the forecaster’s probability distribution. • Then a score is consistent with the directive if that score is minimised by forecasting using that directive. For example if the directive is ‘forecast the mean’ for a continuous variable, then mean square error is a consistent score as it is minimised by forecasting the mean.

  19. Consistent scores - remarks • The assumption of how the forecaster behaves (forecast deterministically when his/her beliefs are probabilistic) implies that the forecaster always hedges in the sense that true beliefs are not forecast. • However, it is the opposite of hedging in its everyday usage (make forecasts less definite), and is not done to improve a score. • As a slight digression, Murphy (1978) argues that ‘the desire to eliminate hedging should encourage forecasters to express … forecasts in probabilistic terms’. • It seems to me that the definition of consistency could be turned around to say that a directive is consistent with a score, rather than a score consistent with a directive. Given any score, if we can find its consistent directive we can reverse the definition again to say that the score is consistent.

  20. Hedging for deterministic forecasts • First, what do we mean by hedging? • For probability forecasts it implies improving ‘expected score’. But expectation is with respect to the forecaster’s true beliefs. • For deterministic forecasts either the forecaster’s true beliefs are • Deterministic (and clearly wrong) or • Probabilistic and unknown. • So does hedging now imply improving actual score? Or is there another definition?

  21. Back to equitability • Although apparently not very useful for probability forecasts, equitability is often made a requirement for deterministic categorical forecasts. • Does equitability rule out hedging when hedging implies improvement of actual score? • Does non-equitability necessarily imply that a score can be hedged?

  22. Equitability – a conjecture • Equitability ensures that hedging is impossible for deterministic categorical forecasts. • It works for the Peirce skill score, an equitable score for binary forecasts • Transferring a proportion of forecasts of an event to forecasts of no event or, conversely, transferring a proportion of no-event forecasts to ‘event’, reduces the Peirce skill score. • But is this the only way that a forecaster can diverge from his/her true beliefs?

  23. Non-equitable scores • Non-equitable scores may or may not be hedged, depending on details of the data • Consider ‘Proportion Correct’ in a (2x2) table, a non-equitable score, (a+d)/n • If a>b and d>c the score cannot be improved by transferring a proportion of forecasts to non-forecasts, or vice versa; otherwise it can. For the tornados, a < b, so PC can be hedged.

  24. Questions? Or answers!

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