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GOES-R AWG Aviation Team: Flight Icing Threat (FIT) June 14, 2011

GOES-R AWG Aviation Team: Flight Icing Threat (FIT) June 14, 2011. William L. Smith Jr. NASA Langley Research Center Collaborators: Patrick Minnis, Louis Nguyen NASA Langley Research Center Cecilia Fleeger, Doug Spangenberg, Rabindra Palikonda SSAI@ NASA Langley Research Center. Outline.

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GOES-R AWG Aviation Team: Flight Icing Threat (FIT) June 14, 2011

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  1. GOES-R AWG Aviation Team: Flight Icing Threat (FIT)June 14, 2011 William L. Smith Jr. NASA Langley Research Center Collaborators: Patrick Minnis, Louis Nguyen NASA Langley Research Center Cecilia Fleeger, Doug Spangenberg, Rabindra Palikonda SSAI@ NASA Langley Research Center

  2. Outline • Executive Summary • Algorithm Description • ADEB and IPR Response Summary • Requirements • Validation Strategy • Validation Results • Summary

  3. Executive Summary • This ABI Flight Icing Threat (FIT) detection algorithm generates an Option 2 product. • ATBD (100%) and Software Version 5 are on track for delivery for a July delivery. • Algorithm utilizes ABI cloud products to identify areas icing is likely to occur and estimates the probability for icing in two severity categories. • Validation Datasets: Icing PIREPS, TAMDAR, and ground-based icing remote sensing data. • Validation studies indicate that the product is meeting spec.

  4. Algorithm Description In-flight Aircraft Icing depends on • presence of super-cooled liquid water (SLW) • liquid water content, LWC • Droplet size distribution, N(r) • Temperature, T(z) GOES-R ABI can provide • Cloud top temperature and phase: SLW • liquid water path:LWP = f(LWC) • effective radius,re = f(N(r)) Satellites detect icing conditions

  5. Algorithm Description Map satellite-derived cloud parameters to Flight Icing Threat Exploit high horizontal and temporal resolution 300 Effective Radius (μm) 0 100 200 600 800 Cloud Top Phase Liquid Water Path (g/m2) 0 5 7 9 11 13 15 17 19 21 25 Approach • Match ABI proxy cloud products with Pilot reports of icing and determine relationships • Use NASA LaRC GOES products for prototype method/initial validation • Tune technique for ABI (MODIS proxy with CAT products) Icing PIREPS

  6. Algorithm Summary • The flight icing threat is determined using theoretically based cloud parameter retrievals. • The icing mask is first constructed (icing, none, unknown) using the cloud phase and optical depth (day and night). • The IR-only approach used by the CAT for Cloud Phase provides day/night consistency and takes advantage of the ABI’s improved spectral information (big advance over current GOES). • During daytime, the icing probability and severity are computed for each ‘icing’ pixel using the retrieved LWP and Re. • Additional output parameters include quality control flags and estimates of the icing altitude boundaries. • FIT is indeterminate when high clouds obscure view (see poster for new methods being developed to help alleviate this shortcoming).

  7. SEVIRI RGB 10/16/2009 Flight Icing Threat Processing Schematic INPUT: Cloud Phase, Tau, LWP, Re AWG Cloud Phase Determine ‘icing’ pixels (optically thick SLW pixels) Mask the remaining pixels as ‘none’ (cloud free, warm clouds) or ‘unknown’ (optically thick high clouds) AWG Liquid Water Path Clear Liquid Ice Mixed SLW During daytime, estimate icing probability and severity from LWP, Re for icing pixels Output Icing Mask and Index 400 600 800 1000 0 200

  8. Flight Icing Threat Product Output CURRENT GOES Daytime Nighttime

  9. Algorithm Changes from 80% to 100% • Developed method to scale LWP to S-LWP for clouds that extend below freezing level. • Requires knowledge LWC(z), the freezing level (NWP) and the cloud geometric thickness (NASA LaRC parameterization). • Four LWC (Z) distributions: (1) Uniform LWC(z), (2) Adiabatic LWC(z) – inc w/altitude (3) dec w/altitude, (4) Climatology (from CloudSat) are being tested. • Added Icing Altitude Boundaries (Ztop from ACHA, Zbase from Ztop - ΔZ or freezing level, whichever is higher. • Adding snow cover dependence (requires dynamic snow map). • Metadata output added. • Quality flags standardized. 9

  10. Summary of ADEB and Independent Peer Review (IPR) Feedback • Main issues from IPR • Concern regarding the usefulness of the accuracy requirement • - Agree but icing definition ill-defined (more later). • Concern regarding the dependence on unproven ABI cloud products and consistency with LaRC products used in prototype • ABI products are looking reasonable and are being validated and compared to legacy products. We are working with CAT understand differences. The FIT can be tuned to the ABI cloud products. ABI-FIT validation will determine what level of algorithm tuning is needed, if any.

  11. Summary of ADEB and Independent Peer Review (IPR) Feedback • All ATBD errors and clarification requests have been addressed. • No feedback required substantive modifications to the approach. • ADEB would like to see more validation with TAMDAR • - We agree and are working with AIRDAT to acquire additional TAMDAR datasets

  12. Requirements

  13. Validation Approach

  14. Validation Approach: Datasets • Icing PIREPS • Match satellite pixels within 20km and +/- 15 minutes of each PIREP • TAMDAR icing sensor on ~400 commercial aircraft • 4 closest pixels, +/- 15 minutes matched to each observation • NIRSS - Ground-based icing remote sensing products at NASA GRC, Cleveland, OH • Match pixels within 20km of site and avg NIRSS data (time, altitude) 14

  15. Validation Approach: Qualifier • Truth datasets each have their own associated uncertainties and limitations • PIREPS (geolocation errors, biased, severity subjective) • TAMDAR (‘no icing’ can be ambiguous due to sensor issues and knowledge of presence ‘in-cloud’ • NIRSS a remote sensing concept, not direct PODY (skill in positive detection) reliable but PODN, False Alarms difficult to ascertain and not meaningful. NIRSS could help. 15

  16. Validation Approach: Qualifier • There is currently no accepted definition of severity by cloud microphysics parameters (e.g LWC, Re) or accretion rate on an airplane (considering the variety of airplanes and their aerodynamics, this would also carry some uncertainty), thus PIREPS, etc will have to do FIT Severity validation and calibration are difficult 16

  17. Validation Results Current GOES (LaRC Cloud Algorithms) Validation with PIREPS: Flight Icing Threat Numerous Icing PIREPs confirm ABI flight icing threat Use data from several winters

  18. Probability of Detecting Light/Moderate Icing PIREPS L M 3346 992 L Satellite 1498 2633 M POD(light) = 55% POD(mdt) = 60% Validation with PIREPSWinter 2008-2010 Probability of Detecting Icing PIREPS Y N Y • • Algorithm developed with with independent data (3700 PIREPS: winter 2006-2008 • Excellent detection of icing conditions (overcast SLW scenes) • • False reports common, but small % of total • - ‘No Icing’ not reported often 6229 442 Satellite 5 3 N PODY = 99.9% CSI= 93% FAR=7% SS= 99.8% SS = (YY – NY) / (YY +NY) skill in positive detection • Classification of severity has skill but not as much as icing detection • Icing severity often subjective & depends on A/C

  19. Validation Approach: NIRSS NASA Icing Remote Sensing System LWP and Cloud Boundaries (Reehorst et al. 2009) MWR NIRSS approach takes data from microwave radiometer, cloud radars, experience/data from aircraft icing program to derive super-cooled LWC profiles which can be mapped to icing severity profiles Cloud Radars Ground-based Sensors at NASA GRC Icing Severity profiles Convert LWC to Severity Tuned to airfoil model (Politovitch 2003) 19 19 19 19

  20. Probability of Detecting Light/Moderate Icing PIREPS L M 145 (144) 30 (19) L Satellite 16 (27) 41 (42) M PODL = 78 (77) % PODM = 35 (59)% Validation with NIRSSWinter 2008-2010 Probability of Detecting Icing PIREPS Y N Y 232 17 Satellite • • Similar detection skill as found using PIREPS • Need more data (coming soon) 0 0 N PODY = 100% CSI= 93% FAR=7% SS= 100% SS = (YY – NY) / (YY +NY) skill in positive detection FIT V5 (V3) • Classification of severity good for V3. Not as good for V5 • -FIT algorithm is tuned to PIREPS • - NIRSS tuned to airfoil model

  21. Flight Icing Threat Product Output Oct 16, 2009 (1400 UTC) SEVIRI Phase FIT LWP AIT Framework tests work as expected

  22. Flight Icing Threat Product Output Oct 16, 2009 (1400 UTC) SEVIRI Flight Icing Threat RGB AWG Cloud Phase x Clear Liquid Ice Mixed SLW x X – MDT Icing PIREPs confirm ABI icing threat

  23. Validation Results MODIS (ABI Cloud Algorithms) 16 MODIS granules have been run by the CAT to test FIT and validate with PIREPS 23 NOV 09 25 NOV 09 6 FEB 10 19 DEC 10

  24. Validation Results MODIS (ABI Cloud Algorithms) 16 MODIS granules have been run by the CAT to test FIT and validate with PIREPS 23 NOV 09 25 NOV 09 6 FEB 10 19 DEC 10 24

  25. Validation Summary (Ver 5)

  26. Summary • The ABI Flight Icing Threat algorithm provides a new capability for objective detection of the in-flight icing threat to aircraft • Version 5 software and 100% ATBD on track for delivery in July • Improved ABI spectral coverage, spatial and temporal resolution should offer better detection capability over current GOES particularly at night • Algorithm meets all performance and latency requirements. Some tuning probably required for ABI for severity component • Have not yet quantified missed detection due to cloud phase errors • We are working closely with Cloud Team to acquire ABI cloud products, on cloud product validation, FIT algorithm tuning and validation • 30-40% of atmospheric icing still undetected due to high cloud obscuration (not accounted for in validation). See poster for potential solutions

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