Verification and Metrics (CAWCR)

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Verification and Metrics (CAWCR). Purpose – beyond forecast products. Through the application of appropriate verification methods we: Define the skill of predicting Australian climate on intra-seasonal timescales (forecast products) - PowerPoint PPT Presentation

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The Centre for Australian Weather and Climate ResearchA partnership between CSIRO and the Bureau of Meteorology

Verification and Metrics (CAWCR)

Through the application of appropriate verification methods we:

• Define the skill of predicting Australian climate on intra-seasonal timescales (forecast products)

• Examine the impact of initialisation; ensemble generation and model development on forecast skill

• Diagnose/understand mechanisms and sources of predictability

• Monitor in real-time

Purpose – beyond forecast products

Variables- Precipitation (ensemble mean anomaly; tercile catagories)- Tmax (ensemble mean anomaly; tercile catagories)- Tmin (ensemble mean anomaly; tercile catagories)- SST (ensemble mean anomaly)- MJO RMM indices- Monsoon onset- Other key indices (SAM, blocking)

Stratification- Season (DJF; MAM; JJA; SON)- According to state of ENSO/IOD/SAM/MJO (degree of stratification possible depends on sample size)

Lead time and averaging period- Daily (usually done for prediction of indices)- Fortnight 1 - Fortnight 2- Month 1

Reference forecast- Persistence of observed- Climatology

Leave-one-year-out cross validation (verification of hindcasts)

Comparing systems with different ensemble sizes

Probabilistic scores- Reliability (attributes ) diagram (including frequency histogram)

Dichotomous (yes/no) forecastsConditioned on the fc: given the fc, what was the outcome Reliability, resolution, sharpnessAggregation over region/seasonsNeed fairly large sample (enough cases in each bin)Choice of bin width

- ROC curve Dichotomous (yes/no) forecastsConditioned on obs: given the outcome, what was the fc Resolution (discrimination)Aggregation over region/seasons

- ROC area Grid-point basis and showing significance: determined using the

Mann–Whitney U statistic (Mason and Graham, 2002; Wilks, 2006).

- Brier Skill Score (w.r.t. climatology) Debiased BSS (bias correction for small ensemble size) BBSd - based on weighting of indiv models for MME (not done this yet)

Decomposition of BS: BSrel and BSres components

“Deterministic” scores- Correlation of ensemble mean (usually use temporal rather than spatial)- RMSE ensemble mean- Spread of ensemble

Examples: Rainfall over Australia (Sep/Oct/Nov, fortnight 2)

Reliability diagram

ROC curve

ROC area

Brier skill score

Correlation

BSresROC A

BSrel