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Reliability Trends of the Reliability Trends of the Global Forecast System Global Forecast System Model Output Statistical Model Output Statistical Guidance in the Guidance in the Northeastern U.S. Northeastern U.S. A Statistical Analysis with Operational Forecasting Applications John M. Goff National Weather Servic Burlington, VT

Reliability Trends of the Global Forecast System Model Output Statistical Guidance in the Northeastern U.S. A Statistical Analysis with Operational Forecasting

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Reliability Trends of the Global Reliability Trends of the Global Forecast System Model Output Forecast System Model Output

Statistical Guidance in the Statistical Guidance in the Northeastern U.S.Northeastern U.S.

A Statistical Analysis with Operational Forecasting Applications

John M. GoffNational Weather ServiceBurlington, VT

How is Skill Measured in How is Skill Measured in Probabilistic Precipitation Probabilistic Precipitation

Forecasting (PoP)?Forecasting (PoP)?

A commonly used method of gauging PoP forecasting skill is through the Brier Score (Brier 1950).

1

BS = 1/n (yk – ok)2

k =1

Measuring PoP Forecast Skill Measuring PoP Forecast Skill ContinuedContinued

The Brier Score is analogous to the Mean Squared Error of the PoP forecast and thus is a measure of accuracy.

Measuring PoP Forecast Skill Measuring PoP Forecast Skill ContinuedContinued

An equally valuable measure of PoP forecast skill is reliability.

Reliability is a measure of bias, and is a gage of how accurate probability values are assigned (AWS 1978).

When statistical forecasts have little to no bias they are said to be reliable.

Impetus for ResearchImpetus for Research

Noticeable positive (wet) bias noted in GFS reliability scores at Burlington, VT across lower PoP categories (i.e. 0 < PoP 40).

Occurrence appeared to occur at other northeast U.S. sites, especially during

the winter months.

Data Set Information Data Set Information

Three separate data subsets were examined

1) Northeastern U.S. (20 sites)

2) New England (6 sites)

3) Burlington, VT (1 site)

Data Set DomainData Set Domain

Data Treatment and Data Treatment and ProcessingProcessing

Data examined on three time scales andgathered from NWS verification website.

- Two year period from October 2000 to September 2002

- Two year combined cool season from October 2000(01) to March 2001(02)

- Two year combined warm season fromApril 2001(02) to September 2001(02)

Data Treatment and Data Treatment and ProcessingProcessing

GFS MOS PoP reliability scores calculated for the first three 12 hour forecast periods.

Three period average scores calculated and plotted for the time periods discussed.

- Low Pop (0 < PoP 40) and high PoP

(60 PoP < 100) trends are analyzed.

GFS Alphanumeric GuidanceGFS Alphanumeric Guidance

12 hour pop guidance

Two Year GFS Reliability Two Year GFS Reliability PlotsPlots

Two Year Data Set ResultsTwo Year Data Set Results

Data SetMean Low PoP

BiasMean High PoP

Bias

Northeast U.S. +5.0 % -5.0%

New England +8.6% -3.8%

Burlington, VT +9.2% -2.1%

Two Year GFS Warm Season Two Year GFS Warm Season Reliability PlotsReliability Plots

Two Year Warm Season Data Two Year Warm Season Data Set ResultsSet Results

Data SetMean Low PoP

BiasMean High PoP

Bias

Northeast U.S. +2.9% -5.6%

New England +4.5% -3.6%

Burlington, VT +8.2% -3.8%

Two Year GFS Cool Season Two Year GFS Cool Season Reliability PlotsReliability Plots

Two Year Cool Season Data Two Year Cool Season Data Set ResultsSet Results

Data SetMean Low PoP

BiasMean High PoP

Bias

Northeast U.S. +7.6% -4.0%

New England +12.2% -3.4%

Burlington, VT 10.0% -1.9%

Possible Causes of Observed Possible Causes of Observed TrendsTrends

GFS model coarseness/resolution

GFS MOS PoP regional regression equations

Other error sources- ASOS site location

- Accuracy in precipitation measurement of the ASOS heated tipping bucket (esp. in winter).

GFS MOS PoP Warm Season GFS MOS PoP Warm Season Regression EquationsRegression Equations

GFS MOS PoP Cool Season GFS MOS PoP Cool Season Regression EquationsRegression Equations

Applicability of Results to Applicability of Results to Operational PoP ForecastingOperational PoP Forecasting

By slightly lowering GFS MOS PoP forecasts across lower PoP categories, bias may be reduced (esp. across interior northeast/New England during winter).

Discreet adjustment of GFS MOS PoP forecasts across higher PoP categories is not

recommended (limited number of events).

Applicability to PoP Applicability to PoP Forecasting ContinuedForecasting Continued

This seems to contradict traditional Brier Score theory that hedging PoP forecasts towards the middle probabilities offers a higher probability of success over the long run (Hughes 1980).

Potential Brier Score Points Won/Lost over GFS PoP Guidance for New England Sites

(Mean two year data set values for first three 12 hour forecast periods )

GFS guidance PoP 10 20 30 40

Forecast PoP lowered by (%)

5 10 10 10

Mean number of guidance PoP forecasts

per year per site317 270 204 155

Mean observed yearly freq. per site (%)

4.6 9.0 19.1 31.6

Average points won/lost per year

302/135 720/510 825/585 742/637

Potential Brier Score Points Won/Lost over GFS PoP Guidance for New England Sites

(Mean two year cool season data set values for first three 12 hour forecast periods)

GFS guidance PoP 10 20 30 40

GFS PoP lowered by (%)

5 10 10 10

Mean number of guidance PoP forecasts

per season per site143 130 105 80

Mean observed seasonal freq. per site

2.8 7.7 14.3 27.5

Average points won/lost per season

139/36 360/170 450/225 406/286

OverviewOverview

GFS MOS PoP shows consistent positive bias at lower PoP categories across the northeastern U.S.

Lower associated bias was observed across higher PoP categories.

Overview Contd.Overview Contd.

Possible causes of the observed trends include…

- Coarseness in model resolution- Design of the GFS MOS Pop regional

regression equations- ASOS site location and accuracy of

measurement techniques (esp. in winter)

Overview Contd.Overview Contd.

It is suggested that by lowering GFS PoP forecast values by 5 to 10 percent across lower PoP categories, overall bias may be reduced at many interior northeast and New England sites…especially in winter.

ConclusionsConclusions

Despite noted trends the study was of limited temporal and physical constraints.

Further research on these and/or other sites across the U.S. is needed to ascertain whether trends are inherent within the GFS MOS PoP scheme.

AcknowledgementsAcknowledgements

The author would like to thank Paul Sisson (SOO WFO BTV) for guidance and oversight.

Thanks is also given to Mark Antolik of MDL for guidance and expertise in the GFS MOS PoP scheme.