Update on CoSPA Storm Forecasts

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Update on CoSPA Storm Forecasts Haig August 2, 2011 This work was sponsored by the Federal Aviation Administration under Air Force Contract No. FA8721-05-C-0002. Opinions, interpretations, conclusions, and recommendations are those of the authors and are not necessarily endorsed by the United States Government. 2011 AMS ARAM 1

CoSPA Precipitation Forecast Deterministic forecast Display: Precipitation (VIL) Echo Tops Horizontal resolution: 1 km (0-2 hour) 3 km (2-8 hr) CONUS coverage Forecast out to 8 hours Time steps: 5 min (0-2 hr) 15 min (2-8 hr) Tactical and strategic planning tool for Traffic Flow Management 2011 AMS ARAM 2

CoSPA 0-8 Hour Forecast Main Components Corridor Integrated Weather System (CIWS) Blending Module High Resolution Rapid Refresh (HRRR) VIL Analysis & Extrapolation Fcsts Blending Weights (X,Y) Extrapolation & Nowcast Model Calibration & Phase Correction Numerical Weather Prediction Model 0 Hour 2 Hour 6 Hour 8 Hour Forecast Lead 2011 AMS ARAM 3

Outline CIWS extrapolation/ nowcast improvements: Improved satellite convective initiation Added Echo Top decay; improved ET growth Improved storm extrapolation HRRR improvements: Replaced RUC with Rapid Refresh (RR) as parent model for HRRR Used reduced diffusion and raised pressure top in HRRR Used finer resolution sea surface temperature field Blending improvements: Added regionally-varying and continually-updating calibration ( running climatology) Improved convective initiation Improved methodology for phase correction Application of CoSPA to probabilistic forecasts 2011 AMS ARAM 4

Nowcast Improvements Satellite Convective Initiation Visible Satellite Incorporated NASA s SATellite Convection AnalysiS and Tracking (SATCAST*) system in FAA CIWS SATCAST performs: Cloud classification Cloud tracking Trending of IR channels IR channel differencing # of SATCAST CI Indicators 8 7 8 satellite-based interest fields indicate confidence in CI Account for cloud growth, glaciation, cloud top height *Mecikalski and Bedka, MWR (2006) 6 5 4 3 2011 AMS ARAM 5

Nowcast Improvements Satellite Convective Initiation Fuzzy Logic CI Nowcast Model Instability Radar Growth Random Forest Predictor Importance Less Important Solar Angle SATCAST Indicators CI Interest CIWS Forecast Engine VIL Forecast CI 40 km away from storm CI within 40 km of storm More Important RF Source: John Williams, NCAR 2011 AMS ARAM 6

Nowcast Improvements Convective Initiation Forecast Example 24 June 2011 2011 AMS ARAM 7

Nowcast Improvements Satellite Convective Initiation 2010 CIWS 1 Hr Precipitation Forecast 2011 CIWS 1 Hr Precipitation Forecast Truth 2010 CIWS 1 Hr Binary Scores 2011 CIWS 1 Hr Binary Scores VIP Level 2 Scores Valid 19 UTC 24 June 2011 HIT MISS FALSE ALARM 2011 AMS ARAM 8

Nowcast Improvements Echo Top Growth and Decay 1400 Z 1500 Z 1600 Z Less Lightning 9 September 2008 Combine trends in lightning and ET to improve ET forecasts 2011 AMS ARAM 9

ET Growth and Decay Predictor Interest Images Filtered Echo Tops above 30kft over Time Echo Tops Trends Lightning Trends Filtered Lightning Flashes over Time 50kft GROWTH 45kft 40kft Combined Trends 35kft 30kft Time Averaged Trends 25kft DECAY 20kft 15kft 10kft 5kft Filtered Trends 0kft 2011 AMS ARAM 10

Nowcast Improvements Echo Top Growth and Decay 2010 CIWS: +2Hr ETF 2011 CIWS: +2Hr ETF ET Truth 0430 +2Hr 0430+2Hr 0630 2 hr Verification Statistics 0kft 5kft 10kft 15kft 20kft 25kft 30kft 35kft 40kft 45kft 50kft HIT MISS FALSE ALARM NOTE: Verification Threshold 30 Kft 28 June 2010 2011 AMS ARAM 11

Extrapolation Improvements Multiscale Storm Advection Radar Track Vectors Cell Envelope Synoptic Wx Classification 13 km Circular Mean Filter 6 Minute Correlation Time 69x13 km Rotated Elliptical Filter 18 Minute Correlation Time 201x101 km Rotated Elliptical Filter 45 Minute Correlation Time 13 km 69x13 km 201x101 km Automated Data Quality Editing Spatial Interpolation Motion Extrapolation (Advection) Motion Data Reference vecs Input vecs Model Winds Multiple scales tracked (cell, envelope, synoptic), rotational & translational motion applied CIWS and CoSPA now share the same advection algorithm 2011 AMS ARAM 12

Extrapolation Improvements Multiscale Storm Advection 2010 CIWS Forecast 2011 CIWS Forecast Truth Level 2 Binary Scores 2010 CIWS +120min 2011 CIWS +120min 2hr CSI Scores 2010 CIWS 2011 CIWS Dayton Area CONUS 21.5 15.4 24.4 16.0 10 May 2011 2015 UTC 2011 AMS ARAM 13

Outline CIWS extrapolation/ nowcast improvements: Improved satellite convective initiation Added Echo Top decay; improved ET growth Improved storm extrapolation HRRR improvements: Replaced RUC with Rapid Refresh (RR) as parent model for HRRR Used reduced diffusion and raised pressure top in HRRR Used finer resolution sea surface temperature field Blending improvements: Added regionally-varying and continually-updating calibration ( running climatology) Improved convective initiation Improved methodology for phase correction Application of CoSPA to probabilistic forecasts 2011 AMS ARAM 14

HRRR Improvements RR Parent and Diffusion 2010 RUC Parent Strong LH 6 th Diffusion 2011 RR Parent Strong LH No 6 th Diffusion 12Z + 9h forecast valid 21z 17 July 2010 NSSL Verification 21 UTC Better SE coverage for RR parent with no 6 th order diffusion 2011 AMS ARAM 15

HRRR Improvements RR Parent and Diffusion 2010 RUC Parent Strong LH 6 th Diffusion 25 dbz 40-km East CSI =.16 bias=1.21 NSSL Verification 21 UTC 2011 RR Parent Strong LH No 6 th Diffusion 25 dbz 40-km East CSI =.20 bias=1.50 12Z + 9h forecast valid 21z 17 July 2010 HRRR: Paper 13.2 Alexander, NOAA GSD 10:45AM Thu 2011 AMS ARAM 16

Outline CIWS extrapolation/ nowcast improvements: Improved satellite convective initiation Added Echo Top decay; improved ET growth Improved storm extrapolation HRRR improvements: Replaced RUC with Rapid Refresh (RR) as parent model for HRRR Used reduced diffusion and raised pressure top in HRRR Used finer resolution sea surface temperature field Blending improvements: Added regionally-varying and continually-updating calibration ( running climatology) Improved convective initiation Improved methodology for phase correction Application of CoSPA to probabilistic forecasts 2011 AMS ARAM 17

Blending Improvements Regionally Varying Weights Shifted from static to dynamic weights Accounts for regional variations in relative performance Adapts to changes in the skill of the inputs on the fly Improved skill of forecast Model_WT Gen1300_Fcst05h = v1800utc Static Weight = 0.67 Dynamic Weight = 0.35-0.71 Bias, T=133, Eastern US FA2010 SP2011 FA2010 SP2011 Blending Source: James Pinto, NCAR 2011 AMS ARAM 18

Blending Improvements Scale Dependent Merging Weights are a function of time of day, leadtime, and region (where storm initiation is indicated) Identify model initiation areas Implement storm initiation weighting functions Background Weights Model Weights: Storm Init Extrap Storm Init Weights Model Dash : 15 to 00 UTC Solid : 00 to 15 UTC Background Weights 2011 AMS ARAM 19

Blending Improvements Phase Correction Position errors determined using extrapolation forecasts instead of observations Less distortion of storm shapes Improved skill Latency Adj. Summer 2010 Summer 2011 2011 AMS ARAM 20

Outline CIWS extrapolation/ nowcast improvements: Improved satellite convective initiation Added Echo Top decay; improved ET growth Improved storm extrapolation HRRR improvements: Replaced RUC with Rapid Refresh (RR) as parent model for HRRR Used reduced diffusion and raised pressure top in HRRR Used finer resolution sea surface temperature field Blending improvements: Added regionally-varying and continually-updating calibration ( running climatology) Improved convective initiation Improved methodology for phase correction Application of CoSPA to probabilistic forecasts 2011 AMS ARAM 21

Probabilistic Forecast Based on Weather Avoidance Field CIWS WEATHER DATA VIL EchoTop WEATHER AVOIDANCE FIELD 16km Echo Top Maximum Deviation Probability Lookup Table 60km VIL Area Coverage WAF Fcst 1 WAF Fcst 2 WAF Fcst 3 CoSPA-based WAF Forecast Time-lagged Ensemble WAF DEVIATION DATABASE Non-Deviation Deviation Data > Threshold Data < Threshold Center pixel location Probability = # Pixels above threshold Total # pixels in cylinder 2011 AMS ARAM 22

Probabilistic Forecast Display Concepts Probabilistic Contour Underlay Probability of WAF > 30% Spatial Smoothing Sub-Sampled and Smoothed Convective Weather Polygons Processed to Approximate Human Drawn 2011 AMS ARAM 23

Probabilistic Forecast Convective Weather Polygons CCFP CoSPA Polygons 6 - Hr 6 - Hr May provide first guess for CCFP CoSPA polygons being evaluated as part of 2011 Aviation Weather Center Testbed Summer Experiment 2011 AMS ARAM 24

Summary CoSPA received upgrades to all three of its components: CIWS extrapolation, HRRR model, and blending module Upgrades included improved convective initiation, storm decay, storm motion, storm structures Evaluation of CoSPA is taking place this summer Probabilistic convective polygons based on CoSPA forecasts are being evaluated as part of the AWC 2011 Testbed Summer Experiment Acknowledgements: J. Pinto, M. Wolfson, S. G. Benjamin, M. Steiner, S. S. Weygandt, C. Alexander, W. J. Dupree, J. K. Williams, J. R. Mecikalski, W. F. Feltz, K. Bedka, D. Morse, X. Tao, D. A. Ahijevych, C. Reiche, T. Langlois, K. L. Haas, L. J. Bickmeier, P. M. Lamey, J. M. Pelagatti, and D. D. Moradi 2011 AMS ARAM 25