Statistical Postprocessing of LM Weather Parameters Susanne Theis
- Slides: 35
Statistical Postprocessing of LM Weather Parameters Susanne Theis Andreas Hense Ulrich Damrath Volker Renner
Overview - Introduction - Short Description of Neighbourhood Method - Verification Results - Calibration - Concluding Remarks COSMO - 5. Annual Meeting 25. 09. 2003
LM Total Precipitation [mm/h] COSMO - 5. Annual Meeting 08. Sept. 2001, 00 UTC, vv=14 -15 h 25. 09. 2003
Neighbourhood Method Assumption: LM-forecasts within a spatio-temporal neighbourhood are assumed to constitute a sample of the forecast at the central grid point COSMO - 5. Annual Meeting 25. 09. 2003
Definition of Neighbourhood I y t x COSMO - 5. Annual Meeting x 25. 09. 2003
Definition of Neighbourhood II Size of Area Form of Area hs Linear Regressions COSMO - 5. Annual Meeting 25. 09. 2003
Products Probabilistic Information • Quantiles • (Exceedance probabilities for certain threshold values) „Statistically smoothed” fields • Quantiles for p = 0. 5 • Expectation Values COSMO - 5. Annual Meeting 25. 09. 2003
LM Total Precipitation [mm/h] Original Forecast COSMO - 5. Annual Meeting 08. Sept. 2001, 00 UTC, vv=14 -15 h Expectation Values 25. 09. 2003
LM Total Precipitation [mm/h] Original Forecast COSMO - 5. Annual Meeting 08. Sept. 2001, 00 UTC, vv=14 -15 h Quantiles for p=0. 9 25. 09. 2003
LM T 2 m [o. C] Original Forecast COSMO - 5. Annual Meeting 08. Sept. 2001, 00 UTC, vv=15 h Quantiles for p=0. 5 25. 09. 2003
Direct model output of the LM for precipitation at a given grid point COSMO - 5. Annual Meeting 25. 09. 2003
. . . supplemented by more quantiles (forecast of uncertainty) COSMO - 5. Annual Meeting 25. 09. 2003
. . . supplemented by the 90 %-quantile (forecast of risk) COSMO - 5. Annual Meeting 25. 09. 2003
Verification Data LM forecasts; 1. -15. 09. 2001; 00 UTC starting time 1 h values; 6 -30 h forecast time all SYNOPs available from German stations comparison with nearest land grid point NM-Versions small: 3 time levels (3 h); radius: 3 s ( 20 km) medium: 3 time levels (3 h); radius: 5 s ( 35 km) large: 7/3 time levels (7/3 h); radius: 7 s ( 50 km) Averaging square areas of different sizes temperatures adjusted with -0. 65 K/(100 m) COSMO - 5. Annual Meeting 25. 09. 2003
COSMO - 5. Annual Meeting 25. 09. 2003
COSMO - 5. Annual Meeting 25. 09. 2003
Richardson, D. S. , 2001: Measures of skill and value of ensemble prediction systems, their interrelationship and the effect of ensemble size. Q. J. R. Meteorol. Soc. , Vol. 127, pp. 2473 -2489) COSMO - 5. Annual Meeting 25. 09. 2003
COSMO - 5. Annual Meeting 25. 09. 2003
COSMO - 5. Annual Meeting 25. 09. 2003
COSMO - 5. Annual Meeting 25. 09. 2003
COSMO - 5. Annual Meeting 25. 09. 2003
COSMO - 5. Annual Meeting 25. 09. 2003
COSMO - 5. Annual Meeting 25. 09. 2003
COSMO - 5. Annual Meeting 25. 09. 2003
COSMO - 5. Annual Meeting 25. 09. 2003
COSMO - 5. Annual Meeting 25. 09. 2003
COSMO - 5. Annual Meeting 25. 09. 2003
COSMO - 5. Annual Meeting 25. 09. 2003
COSMO - 5. Annual Meeting 25. 09. 2003
COSMO - 5. Annual Meeting 25. 09. 2003
Calibration (addressing the effect of limited sample size only) Based on Richardson (2001) we derive a relation: p' = p' (p, M, m, s) M: effective sample size m, s: related to the parameters of the beta distribution (r, s) COSMO - 5. Annual Meeting 25. 09. 2003
Preliminary Result of Calibration Elimination of m and s Artificial choice: M=10 Reliability diagram of 1 h accumulated precipitation in the period 10. -24. July 2002 (LM forecasts starting at 00 UTC; small version of neighbourhood method) COSMO - 5. Annual Meeting 25. 09. 2003
original forecast small medium large [mm/h] Relative value of precipitation forecasts (original forecast and 90 % quantiles) for users, whose cost/lost ratio is equal to 10 % for the threshold values given by the abscissa COSMO - 5. Annual Meeting 25. 09. 2003
Concluding Remarks “Statistically Smoothed” Fields For temperature no mean advantage is to be seen in comparison with simple averaging The results for precipitation are difficult to judge upon; proper choice amongst the various possibilities is still an open question Reliability Diagrams Possible improvement by calibration remains to be explored The results for the lower quantiles of precipitation indicate the need for improving the model (reduce the overforecasting of slight precipitation amounts) Higher quantiles of precipitation seem to be valuable already without calibration COSMO - 5. Annual Meeting 25. 09. 2003
Concluding Remarks (ctd. ) Outlook • Results of the neighbourhood method will be compared to those of more extensive experimental ensemble integrations • Calibration of quantiles will hopefully be further developed • The method will be tested on the 2. 8 km LM version and compared to other/simpler methods. Application in combination with a small ensemble (LAF) will be investigated • The program has been implemented at Meteo. Swiss and may be made available to other COSMO members COSMO - 5. Annual Meeting 25. 09. 2003
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