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Hydrologic Verification Verification of Deterministic River Stage Forecasts

Edwin Welles OST Seminar June 6, 2007. Hydrologic Verification Verification of Deterministic River Stage Forecasts. 2. Outline of This Talk. Introductory comments about river forecasts. Is there value in verifying stage forecasts?

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Hydrologic Verification Verification of Deterministic River Stage Forecasts

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  1. Edwin Welles OST Seminar June 6, 2007 Hydrologic Verification Verification of Deterministic River Stage Forecasts

  2. 2 Outline of This Talk • Introductory comments about river forecasts. • Is there value in verifying stage forecasts? • Results of evaluating limited sample of NWS stage forecasts. • Proposal: Hydrologists should verify their forecasts. • Results of a hindcasting study on headwater basins. • Proposal 2: We can use verification information to guide our forecast process development. • Standardized Hydrologic Verification • Just advertising

  3. 3 The beneficial ..... and not so beneficial uses of water.

  4. Average Annual Deaths (1990-99): 502 14 99 55 Flood 57 Heat 58 193 26 4 Impacts of Floods and Droughts • Floods kill about 100 people a year • Approximate annual economic losses: Floods - $5 billion Droughts - $6-8 billion

  5. 5 Mitigating the Impacts • Forecasts and data can help us manage our water resources and mitigate the impacts of floods. • NWS started issuing hydrologic forecasts in 1890.

  6. 6 The Approach to River Forecasting Satellite Data Precipitation Estimates River Gage Data Weather Observations Radar Data Models Snow Cover/ Melt Data Precipitation Forecasts Reservoir Releases Climate Predictions Data and Forecasts to Meet Diverse Needs

  7. 7 Forecast Modeling Structure Forecast Point Snow Elevation zone boundary ...for many rivers, Runoff Overland Flow Routing Reservoir with many reservoirs. Channel Routing Rating Curves

  8. 8 The Forecast Process Observed: p, T, PE, Qres, Stg Verification BULLETIN FLOOD WARNING NATIONAL WEATHER SERVICE SHREVEPORT LA 1033 AM CDT WED APR 13 2005 Forecast: p, T, PE, Qres, Q Data Assimilation

  9. 9 Where’s the …..?

  10. Where’s the …..? 10 • … Verification • Little verification of hydrologic forecasts has been conducted to date. • My Main Point • Need to fill this void in both Research and Operations. • So let’s look at some verification metrics

  11. 11 Description of the Data • Two sets of River Stage forecasts from NWS RFCs • OK Dataset • 4 Locations in Oklahoma • 1993 to 2002 • 1 to 4 basins above the forecast point • Response time measured in hours • MM Dataset • 11 locations along the mainstem of the Missouri river • 1983 to 2002 • 500 to 1000 basins above the forecast point • Response time measured in days • Generated a Persistence forecast as a reference • Observation at time of forecast persisted into the future

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  15. 15 Initial Observationsfrom this limited sample • Day 1 and Day 2 forecasts are accurate and skillful (as compared to persistence). • Little skill in day 3 • Little change over the periods of record. • Need to conduct a more complete study to establish a comprehensive baseline so we can answer this basic question. • What is the skill of hydrologic forecasts?

  16. V E R I F I C A T I O N V E R I F I C A T I O N V E R I F I C A T I O N V E R I F I C A T I O N V E R I F I C A T I O N V E R I F I C A T I O N V E R I F I C A T I O N V E R I F I C A T I O N Improving The Approach to River Forecasting 16 Leverage Data and Systems from NOAA and Collaborators Satellite Data Precipitation Estimates River Gage Data Weather Observations Radar Data Models Snow Cover/ Melt Data Precipitation Forecasts Reservoir Releases Valuable Data and Forecasts to Satisfy Diverse Customer Needs Climate Predictions

  17. 17 Some More Basic Questionsfor which we do not have answers • How is new science improving the forecasts? • What are the largest sources of error in the forecasts? • What should be done to improve the forecasts? How can verification can help us answer these questions?

  18. 18 A Hindcasting Experiment to Analyze Sources of Error • Generated hindcasts • Three headwater basisns in Oklahoma and Missouri. • Out to three day lead times • Four years (1997 to 2000) • Twelve total scenarios using… • 2 calibrations • A “good” and an “a priori” calibration • 2 state updating methods • Updated initial conditions and not-updated initial conditions • 3 QPF scenarios • Perfect QPF • The observations • Actual QPF • Computed QPF for 24 hours and then zero for days 2 and 3 • Zero QPF • Zero for all 3 days

  19. 19 Analysis Method • For each scenario • Computed standard verifiction metrics on 4 subsets of the data • Sorted into high and low stages • Sorted by observations and by forecasts • Sorting by observations – Discrimination • Sorting by forecasts – Reliability • Presenting just RMSE for High stage discrimination • Compared scenarios with simple differences between the metrics. • Evaluated error in the QPF also.

  20. 20 Comparing the Calibrations

  21. 21 • The Skill of the Input Forecasts

  22. 22 Comparing the State Updating Scenarios • State updating appears to bring similar skill to the hindcasts as the calibration in the early periods. • QPF and state updating skill appear independent.

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  24. 24 Comparing theCalibration Scenarios • State updating appears to bring similar skill to the hindcasts as the calibration in the early periods. • Improving the calibration may degrade forecast skill depending upon the QPF characteristics. • Need good QPF to realize benefits of improved calibration.

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  26. 26 Comparing the QPF Scenarios • Using some QPF almost always improves the forecasts (1 exception) for the High Stages • Not so for the low stages. • Can capitalize on the improved QPF even with poor calibration. • But get more improvement with better calibration

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  29. 29 Improving The Forecast Process The hindcasts tell us .... Observed: p, T, PE, Qres, Stg Help needed for > day 1 forecasts Verification Verification Verification Verification Verification Verification Verification Verification Verification BULLETIN FLOOD WARNING NATIONAL WEATHER SERVICE SHREVEPORT LA 1033 AM CDT WED APR 13 2005 Verification Forecast: p, T, PE, Qres, Q Data Assimilation Critical for < day 1 forecasts

  30. 30 Standardized Verification for Hydrologic Forecasts This Professor has a really good idea. This one used verification to explain her idea. U N W S U NWS Without Verification With Verification It is hard to communicate without a common language. Standardized Verification is the common language forecasters and researchers need.

  31. 31 Standardized Verification for Hydrologic Forecasts • Supports research by identifying needs AND by clarifying the value of results. • Supports operational agencies by defining acceptable methods. • They are expected to evolve, but we must start somewhere. • Use peer review to establish validity.

  32. 32 Hydrologic Forecast Process Supported by a complete verification system.

  33. 33 Summary • Identified a need • Fill the hydrologic verification void. • Documented an initial description of NWS river stage forecast skill. • Need to verify more forecasts to update baseline • Verification methods can identify sources of error. • Demonstrated with hindcast experiment • Propose Standardized Verification will enhance verification efforts and moving research to operations.

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