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Improving snow nowcasts for airports Elena Saltikoff, Finnish Meteorological Institute (FMI) Seppo Pulkkinen, FMI Annakaisa von Lerber, FMI Martin Hagen, German Aerospace Center (DLR) PNOWWA (Probabilistic Nowcasting of Winter Weather for


  1. Improving snow nowcasts for airports Elena Saltikoff, Finnish Meteorological Institute (FMI) Seppo Pulkkinen, FMI Annakaisa von Lerber, FMI Martin Hagen, German Aerospace Center (DLR) PNOWWA (Probabilistic Nowcasting of Winter Weather for Airports)

  2. Radar 30.11.2017 2

  3. Winter weather

  4. PNOWWA Project Goals Probability This Paper (nr 43 ) distributions Terrain User needs effects Research Paper 36 in this SID Demos A poster in this SID Snowfall. Intensity. Visibility. e.g. Runway Capacity De-icing Throughput Balancing PNOWWA General presentation - Saltikoff

  5. Nowcasting with extrapolation of radar images in PNOWWA Common principle: Time= distance/speed Example: storm 75 km away, moving 50 km/h arrives in 90 minutes ….. dry ……..…… snow...maybe PNOWWA General presentation - Saltikoff

  6. Task split in two In PNOWWA we have tried three 1. Calculate the motion vectors methods for both. and their uncertainty • Simple one from 1990s (Andersson & 2. Move the radar image with the Ivarsson 1991) vectors, assess uncertainty • Operational one from Finnish Met Institute (Hohti et al 2000) • New ones in research (Proesmans et al, Pulkkinen et al. ) • (This picture related to the FMI Operational one: ellipse is related to the uncertainty of motion vectors.) PNOWWA General Presentation - Saltikoff

  7. The Simple Method: Andersson & Ivarsson 1991 Frequency distribution in source area as probability distrubution by time of arrival Uncertainty of movement direction 90-105 min forecast sector estimated as constant +/-30 degrees 850 hPa wind vector PNOWWA

  8. The simple one was used in first demos, and it performed quite well ! EFHK Red: Observations (15 minutes) Green shades: 30-120 min forecasts PNOWWA General Presentation - Saltikoff

  9. Even in Innsbruck, which is a challenging place for radars PNOWWA General Presentation - Saltikoff

  10. ”Radar is an excellent tool to say it is not raining ” Based on this image we can say that the precipitation does not start in EFJY in 2 hours. It is obvious for a EFJY meteorologist*. But it is valuable information for the snowplough driver. *In Finland, in wintertime PNOWWA General Presentation - Saltikoff

  11. Why snow ? Why Airport ? Extrapolation works only Airport is a known point for already existing with limited number of precipitation : you can not professional users forecast summertime afternoon showers in the morning with these methods. PNOWWA General presentation - Saltikoff

  12. Radar better than NWP model up to 2h Helsinki-Vantaa, 15 minutes steps: Hitrate, winters 2015-2016. Colours: Radar-based extrapolation TAF NWP Model 30.11.2017 12

  13. New nowcasting method based on Stochastic Ensembles: STEPS • Motion field from consecutive radar images • Uncertainty of motion assessed from a set of trajectories • Uncertainty due to growth and decay modeled by a stochastic random field PNOWWA General presentation - Saltikoff

  14. A radar image is decomposed to different scales Large Medium Smallest Long-living features Inbetween To be quickly replaced which move as they are with random noise , smoothed out in output PNOWWA General Presentation - Saltikoff

  15. STEPS: Forecast Ensembles and Probabilities Nowcast +15 minutes +30 minutes +5 minutes Ensemble mean Members • 51 ensemble members are obtained by perturbing precipitation intensities and motion field. • The ensemble mean represents the “most probable” precipitation intensity. • The mean field becomes smoother when the forecast time increases: badly predictable scales are filtered out. • The ensembles also yield probability distributions of precipitation intensities.

  16. Comparing two cases in STEPS (the advanced method). Time step 5 minutes, 60 min range.

  17. Two diagram types ROC – Relative Operating Reliability diagrams Characteristics Perfect Observed FAR frequency Perfect POD Forecasted probability PNOWWA General presentation - Saltikoff

  18. Reliability diagrams Plots observed frequency against the forecast probability, where the range of forecast probabilities is divided into bins ( 0-5%, 5-15%, 15- 25%, etc.). The sample size in each bin is included as a histogram or values. Reliability is indicated by the proximity of the plotted curve to the diagonal. Observed frequency Perfect Forecasted probability PNOWWA General presentation - Saltikoff

  19. Reliability diagram 15 min Laaja Kuurot

  20. Reliability diagram 30 min Laaja Kuurot

  21. Reliability diagram 60 min In the isolated showers In widepread case, when 40-80% was case, even 60 min forecast forecasted, almost 100% happened: almost perfect ! underforecasting Laaja Kuurot Small probabilities forecasted so seldomly, that this measure is not reliable

  22. ROC – Relative Operating Characteristics Plot hit rate or probability of detection against false alarms using set of increasing probabilities to make a yes-no decisions. Diagonal: no skill . Over 5% prob Larger area above diagonal: Larger skill = yes, snow ! Perfect POD Over 80% prob = yes, snow ! FAR PNOWWA General Presentation - Saltikoff

  23. ROC 15 min

  24. ROC 30 min PNOWWA General presentation - Saltikoff

  25. ROC 60 min Still very high Probability of Still very low false alarm rate Detection

  26. This was all radar-to-radar Radar reflectivity is a measure of For dBZ, one 2 mm snowflake sum of diameters of particles in contributes as much as 64 snow power of six. flakes of 1 mm – for visibility not. So, it is related to • Number of snowflakes in volume • Size of snowflakes in volume • Other microphysical properties (dielectricity) of the snowflakes Visibility and snow depth are also related to these parameters. But the relationship is not straightforward. PNOWWA General Presentation - Saltikoff

  27. A lot of variability From dBZ to visibility Snow ratio: from mm to cm PNOWWA General Presentation - Saltikoff

  28. Scandinavian ” mountains ” PNOWWA General Presentation - Saltikoff

  29. Mountains It’s complicated. Results from hills in Scandinavia do not apply to real mountains of the Alps. Motion vectors from radar data or the upper level wind do not explain why fronts sometimes stop. Future: analysis of motion vector uncertainty to assess cyclogenesis PNOWWA General presentation - Saltikoff

  30. Forecasting with thresholds • Final Probability for over 5 mm selection Probability for • If not, then more 1-5 mm or less? How many • Not accurate anyways millimeters PNOWWA General presentation - Saltikoff

  31. Potential for follow-up projects as identified in PNOWWA Surveys PNOWWA is S2020 Fundamental Numerical Explonatory Research. To reach higher Weather maturity levels, more Prediction work is needed Models (EPS) Data Special models (road, Fusion fog , DRSN, …) Annex III standard products (TAF, METAR, …) PNOWWA General Presentation - Saltikoff

  32. Snow at airport Aviation users are not afraid of probabilities Radar is a useful tool for nowcasting • Timing in steps of 15 minutes • Lead times up to 2-3 hours It is also important to forecast that it will not snow PNOWWA General Presentation - Saltikoff

  33. PNOWWA Probabilistic Nowcasting of Winter Weather for Airports Thank you very much for your attention! This project has received funding from the SESAR Joint Undertaking under the European Union’s Horizon 2020 research and innovation programme under grant agreement No 699221 The opinions expressed herein reflect the author’s view only. Under no circumstances shall the SESAR Joint Undertaking be responsible for any use that may be made of the information contained herein.

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