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Beth Ebert Bureau of Meteorology Research Center Melbourne, Australia PowerPoint Presentation
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Beth Ebert Bureau of Meteorology Research Center Melbourne, Australia

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  1. Monitoring the Quality of Operational and Semi-Operational Satellite Precipitation Estimates – The IPWG Validation / Intercomparison Study Beth Ebert Bureau of Meteorology Research Center Melbourne, Australia 2nd IPWG Meeting, Monterey, 25-28 October 2004

  2. Motivation – provide information to... • Me...! fill the blank spot • Algorithm developers • How well is my algorithm performing? • Where/when is it having difficulties? • How does it compare to the other guys? • Climate researchers • Do the satellite rainfall products give the correct rain amount by region, season, etc? • Hydrologists • Are the estimated rain volumes correct? • NWP modelers • Do the satellite products put the precipitation in the right place? • Is it the right type of precipitation? • Forecasters and emergency managers • Are the timing, location, and maximum intensities correct?

  3. http://www.bom.gov.au/bmrc/wefor/staff/eee/SatRainVal/sat_val_aus.htmlhttp://www.bom.gov.au/bmrc/wefor/staff/eee/SatRainVal/sat_val_aus.html Web page for Australia – home

  4. Earlier studies GPCP Algorithm Intercomparison Programs (AIPs) and WetNet Precipitation Intercomparison Programs (PIPs) found: • Performance varied with sensor • Passive microwave estimates more accurate than IR and VIS/IR estimates for instantaneous rain rates • IR and VIS/IR slightly more accurate for daily and monthly rainfall due to better space/time sampling • Performance varied with region and season • Tropics better than mid- and high latitudes • Summer better than winter (convective better than stratiform) • Model reanalyses performed poorer than satellite algorithms for monthly rainfall in tropics, but competitively in mid-latitudes (PIP-3)

  5. More recent studies • Combination of microwave and IR gives further improvement at all time scales • Good accuracy of microwave rain rates • Good space/time sampling from IR (geostationary) • Strategies • Weighted combination of estimates • Using match-ups of microwave and geostationary estimates • Get a field of multiplicative correction factors • Tune parameters of IR algorithm • Map IR TB onto microwave rain rates • Morphing of successive microwave estimates using time evolution from geostationary imagery • Paradigm for GPM?

  6. Focus of IPWG validation / intercomparison study • Updated evaluation of satellite rainfall algorithms

  7. Quantitative Precipitation Forecasts (QPFs) from Numerical Weather Prediction (NWP) • WCRP Working Group on Numerical Experimentation (WGNE) has been validating / intercomparing model QPFs since 1995 • Results • Performance varies with region and season • Mid-latitudes better than tropics • Winter better than summer (stratiform better than convective) • NWP performance is complementary to satellite performance! NWP performance over Germany

  8. Foci of IPWG validation / intercomparison study • Updated evaluation of satellite rainfall algorithms • Where, when, under which circumstances is NWP rainfall better than satellite rainfall, and visa versa?

  9. Related studies http://rain.atmos.colostate.edu/CRDC/

  10. Related studies http://ldas.gsfc.nasa.gov/GLDAS/DATA/precip_valid.shtml Observed Precipitation Validation

  11. Parameters of study • Evaluate estimates for at least one year to get seasonal variations in performance • As many different regions (climate regimes) as possible • So far: • Australia • United States • Western Europe • Any volunteers for Asia? Elsewhere? • Focus on daily rainfall • Rain gauge and radar rainfall analyses used as reference data • Focus on relative accuracy • Global estimates archived at U. Maryland

  12. Algorithms • Operational and semi-operational algorithms • Run every day • Available to public via web or FTP • Experimental algorithms OK • Sorted by sensor type • Microwave • IR or VIS/IR • Microwave + IR • Blending strategy NWP models • Global models (ECMWF, US) • Lower spatial resolution, global coverage • Regional models • Higher spatial resolution, limited coverage

  13. Evaluation methodology • Daily rainfall estimates of • Rain occurrence • Rain amount • Spatial resolution • Finest possible resolution (typically 0.25° lat/lon) • Coarser resolution (1° lat/lon) for comparison with NWP • Stratify by • Season • Region • Algorithm type • Algorithm • Rain amount threshold

  14. Verification methods • Rain occurrence • Frequency bias • Probability of detection and false alarm ratio • Equitable threat score • Rain amount • Multiplicative bias • RMS error • Correlation coefficient • Probability of exceedance • Properties of rain systems • Contiguous Rain Area (CRA) validation method (Ebert and McBride, 2000) • Rain area, volume, maximum amount • Spatial correlation • Error decomposition into volume vs. pattern

  15. Some results for Australia...

  16. User page • Targeted to external users of satellite rainfall products

  17. Developer page • Targeted to algorithm developers – contains more algorithms, some of which aren't publicly available (at least not easily)

  18. Multi-algorithm maps • All algorithms and NWP models for 30 September 2004 over Australia

  19. Basic daily validation product • Maps and statistics

  20. Daily CRA validation • Properties of rain system • Area • Mean and maximum rain accumulation • Rain volume • Spatial correlation • Error decomposition into volume and pattern error components

  21. Monthly and seasonal summaries • Variety of statistical plots • Time series • Scatter plots • Table of statistics • Binary (categorical) scores as a function of rain threshold • Error as a function of estimated (observed) rain rate

  22. Intercomparison of algorithm types Australian Tropics Australian Mid-latitudes Multiplicative bias December 2002-September 2004 1° grid summer autumn winter spring

  23. Intercomparison of algorithms Australian Tropics Australian Mid-latitudes POD December 2002-September 2004 1° grid

  24. Caveats • Reference data (gauge and radar analyses) are not as accurate as targeted ground validation sites • Performance results more meaningful in a relative sense than in an absolute sense • No ocean validation • Microwave algorithms are expected to have better performance over ocean because emission signal is used • Therefore microwave+IR algorithms should also perform better over ocean • NWP QPFs perform better over land than over ocean since more observations used in model initialization • Not all algorithms cover the same period (some missing data)

  25. Future of this study • Results so far will be examined closely and written up for publication • Satellite precipitation validation / intercomparison will continue into the future... • Algorithm developers • Keep making your results available • Good opportunity to check new or updated algorithms • Reference data providers • Thanks for data currently provided • More is better! • Can you assist in the validation itself? • Users of validation results • Are we giving you the information you need? • Please provide feedback and suggestions for improvement