Flight Data Analysis Using Limited Data Sets

Similar documents
E230 Aircraft Systems

NATIONAL TRANSPORTATION SAFETY BOARD Office of Research and Engineering Vehicle Performance Division (RE60) Washmgton, D.C

Deriving Meteorological Data from free-to-air Mode-S broadcasts in an Australian Context.

Data evaluation of BDS registers from airborne transponders

Learning. Goals. of pressure. aircraft. Altimeter knob. Page 1 of 8. Document : V1.1

P474 SYDNEY AIRPORT WIND SHEAR ENCOUNTER - 15 APRIL 2007

DETERMINING THE INFLUENCE OF OUTSIDE AIR TEMPERATURE ON AIRCRAFT AIRSPEED

Safety in Numbers SKYWATCH 497. The affordable original.

EMADDC. towards operational collection of Mode-S EHS observations in Europe

QNH: With this setting set on your altimeter you will be reading altitude above mean sea level based on the local station pressure.

Calibrating the Nano Step-by-Step Using the ECP-100

GRAPHICAL AREA FORECASTS (GAF) feet. Flight Information Region boundary QLD-S NSW-E VIC TAS

CAIRNS AIRPORT CYCLONE PLAN

CAIRNS AIRPORT CYCLONE PLAN

NATIONAL TRANSPORTATION SAFETY BOARD WASHINGTON, D.C.

HEIGHT ALTITUDE FLIGHT LEVEL

QLD-S NSW-E NSW-W VIC TAS. A HEADER giving details of the time of issue and the associated validity period.

MetConsole AWOS. (Automated Weather Observation System) Make the most of your energy SM

Adaptive Binary Integration CFAR Processing for Secondary Surveillance Radar *

Mode-S EHS data usage in the meteorological domain:

Pipistrel ALPHA Trainer

Visual Tutorial. Pitot Static System Simulator. Adobe (formerly Macromedia) Flash Requirements

Friends & Partners in Aviation Weather: Part 135

AOPA. Mitigating Turbulence Impacts in Aviation Operations. General Aviation Perspective

Obtaining Meteorological Data from Aircraft with Mode-S Radars

AFM Supplement. Pages Description Of Revision. IR 4/18/03 All Initial Issue Eugene Bollin

Wind data collected by a fixed-wing aircraft in the vicinity of a typhoon over the south China coastal waters

TRAFFIC,TRAFFIC - 5 O CLOCK LOW - 2 MILES

NATIONAL TRANSPORTATION SAFETY BOARD WASHINGTON, D.C. SAFETY RECOMMENDATION LETTER TO THE FAA dated NOVEMBER 21, 1994, AND RESPONSES.

AFM Supplement. Pages Description Of Revision. IR 6/21/04 All Initial Issue Allan Hamann

Establishment of Space Weather Information Service

A tail strike event of an aircraft due to terrain-induced wind shear at the Hong Kong International Airport

Fly, fly away... and bring back data

A Framework for Dynamical True Altitude Modeling in Aviation. Josaphat A. Uvah. University of West Florida, Pensacola, USA

National Transportation Safety Board Office of Aviation Safety Washington, D.C December 10, 2012 WEATHER STUDY DCA13RA025

Meteorology Aviation Manual

Complementary Use of Airborne Wx Radar & Datalink Graphical Wx

NAVIGATION (1) GENERAL NAVIGATION

FLIGHT INSTRUMENTS. This manual is dedicated only for IVAO Network activities. This document must not be used in real aviation or in others networks.

KMD 550/850 Multi-Function Display Quick Reference For Software Version 01/11 or Later

P1.17 Super-high-resolution Numerical Simulation of Atmospheric Turbulence in an Area of Complex Terrain

USE ALTIMETER SETTING

Appendix X for CAP 437 Offshore Helicopter Landing Areas Guidance on Standards.

Montréal, 7 to 18 July 2014

Weather Technology in the Cockpit (WTIC) Program Program Update. Friends/Partners of Aviation Weather (FPAW) November 2, 2016

Jet Aircraft Propulsion Prof. Bhaskar Roy Prof A M Pradeep Department of Aerospace Engineering Indian Institute of Technology, Bombay

SUMMARY. information from

The first tropospheric wind profiler observations of a severe typhoon over a coastal area in South China

GIS Workshop Data Collection Techniques

SPOT THE PROBLEM. TRAFFIC, TRAFFIC - 5 O CLOCK LOW - 2 MILES

Meteorology in Continuous Descent Operations

Nicolas Duchene 1, James Smith 1 and Ian Fuller 2

A description of these quick prepbufrobs_assim text files is given below.

SAE5-35 Altitude Data System. Installation Manual

Data assimilation of Mode-S MRAR over Slovenia. Benedikt Strajnar

ABOP Global Status: What s Now

WAFS_Word. 2. Menu. 2.1 Untitled Slide

COMPARISON OF DOPPLER LIDAR OBSERVATIONS OF SEVERE TURBULENCE AND AIRCRAFT DATA. S.T. Chan * and C.W. Mok Hong Kong Observatory, Hong Kong

Airplane Instruments 1.1 COMPASS ERRORS compass deviation. acceleration/deceleration error compass turning error

USV TEST FLIGHT BY STRATOSPHERIC BALLOON: PRELIMINARY MISSION ANALYSIS

New Zealand Aeronautical Charting the ArcMap Challenge. Presenter: Beryl Pimblott Explorer Graphics Ltd

Integrated Approach of Risk-based Compliance-based Performance-based Audit and Surveillance Programme

[EN-A-083] Potential Benefits of Speed Control on Delay and Fuel Consumption

B KMD 550/850 Multi-Function Display Quick Reference For Software Version 01/14 or Later

VENUS: DETAILED MAPPING OF MAXWELL MONTES REGION

The Importance of Accurate Altimetry in AEM Surveys for Land Management

Weather Needs for UAS Operations

DISTRIBUTED COMPUTER SYSTEMS

Validation of Mode-S Meteorological Routine Air Report aircraft observations

P3.13 GLOBAL COMPOSITE OF VOLCANIC ASH SPLIT ` WINDOW GEOSTATIONARY SATELLITE IMAGES

International Civil Aviation Organization THIRD MEETING OF THE METEOROLOGICAL REQUIREMENTS TASK FORCE (MET/R TF/3)

ESTIMATING THE RESIDUAL TROPOSPHERIC DELAY FOR AIRBORNE DIFFERENTIAL GPS POSITIONING (A SUMMARY)

Monitoring Radar Mechanical Drive Systems FAA's choice of monitoring solutions

ANNEX 23 RESOLUTION MSC.231(82) ADOPTION OF AMENDMENTS TO THE EXISTING MANDATORY SHIP REPORTING SYSTEM IN THE GULF OF FINLAND

Advances in weather and climate science

Regional Hazardous Weather Advisory Centres (RHWACs)

Jet Aircraft Propulsion Prof. Bhaskar Roy Prof. A M Pradeep Department of Aerospace Engineering Indian Institute of Technology, Bombay

Montréal, 7 to 18 July 2014

MetConsole LLWAS (Low Level Wind Shear Alert System)

Future Aeronautical Meteorology Research & Development

STUDY UNIT SEVENTEEN GRAPHICAL AIRMAN S METEOROLOGICAL ADVISORY (G-AIRMET)

Event Date(s): 12:01 AM December 8th, 2013 through 2:00 PM December 12th, 2013

Airborne Geophysical Survey Report River Jordan Property

Feasibility Investigation on Reduced-Power Take-off of MA600

Aurora Bell*, Alan Seed, Ross Bunn, Bureau of Meteorology, Melbourne, Australia

The Improvement of JMA Operational Wave Models

NATIONAL TRANSPORTATION SAFETY BOARD WASHINGTON, D.C

Use of Geophysical Software for Interpretation of Ice-Penetrating Radar Data and Mapping of Polar Ice Sheets

HIGH DENSITY EN ROUTE AIRSPACE SAFETY LEVEL AND COLLISION RISK ESTIMATION BASED ON STORED AIRCRAFT TRACKS

Use of lightning data to improve observations for aeronautical activities

Ground-based temperature and humidity profiling using microwave radiometer retrievals at Sydney Airport.

NATS Report: The viability and Safety Benefits of using the Mode-S Barometric Pressure Setting

INTRODUCTION. In March 1998, the tender for project CT.98.EP.04 was awarded to the Department of Medicines Management, Keele University, UK.

and SUMMARY preliminary parameters. 1.1 MET/14-IP/ /15 In line 1.2 WORLD INTERNATIONAL CIVIL AVIATION ORGANIZATION 2/6/14 English only

Whitepaper. All Currency, One Wallet!

NOISE AND FLIGHT PATH MONITORING SYSTEM GOLD COAST QUARTERLY REPORT JANUARY - MARCH 2013

Long term performance monitoring of ASCAT-A

DATA SOURCES AND INPUT IN GIS. By Prof. A. Balasubramanian Centre for Advanced Studies in Earth Science, University of Mysore, Mysore

Your Source for Global Aviation Forecasts

New frequency counting principle improves resolution

Transcription:

Flight Data Analysis Using Limited Data Sets Neil Campbell Australian Transport Safety Bureau Author Biography: Neil Campbell graduated in 1983 with a Bachelor of Engineering degree (Electronics) from the University of Western Australia. In 1986 Neil joined the Bureau of Air Safety Investigation as a flight recorder specialist. During 1998 he was a member of the ICAO Flight Recorder Panel which developed changes to ICAO Annex 6. In February 2000, Neil joined the Corporate Safety Department of Cathay Pacific Airways Limited in Hong Kong. During 2001 and 2002 he held the position of Manager Air Safety. In December 2003 he rejoined the Australian Transport Safety Bureau as a Senior Transport Safety Investigator. ISASI 2004, Campbell, Flight Data Analysis 1

Flight Data Analysis Using Limited Data Sets Neil A. H. Campbell MO3806 1. INTRODUCTION The use of computer graphics to animate Flight Data Recorder (FDR) or Quick Access Recorder (QAR) information is well known. It is a valuable investigation tool as well as a powerful medium to provide communication and education. With newer aircraft the FDR or QAR will record a comprehensive range of parameters that accurately define its performance and operation. However with general aviation aircraft, most helicopters or older-generation air transport aircraft, there may be no FDR and only a limited number of parameters will be recorded by other systems. At the Australian Transport Safety Bureau (ATSB) animations have been produced using limited data sets including: Radar data Global Positioning System (GPS) data Electronic control unit data (eg. engine data) Basic FDR parameters The case study presented in this paper is from a Bell 407 helicopter accident. Two sources of recorded data were available for this investigation: Ground-based Radar data Onboard Electronic Control Unit (ECU) data 2. RADAR DATA 2.1 Background Primary radar returns are produced by radar transmissions which are passively reflected from an aircraft and received by the radar antenna. The received signal is relatively weak and provides only position information. Primary radars, which are only located near capital city airports, have a nominal range of 50 NM. Secondary radar returns are dependent on a transponder in the aircraft to reply to an interrogation from the ground. The aircraft transmits an encoded pulse train containing the secondary surveillance radar (SSR) code and other data. Pressure altitude may be encoded with these pulses. As the aircraft transponder directly transmits a reply, the signal received by the antenna is relatively strong. Consequently, an aircraft which has its transponder operating can be more easily and reliably detected by radar. Civilian secondary surveillance radars are located along the east coast of Australia to meet the operational requirement of radar coverage from 200 NM north of Cairns to 200 NM west of Adelaide. Coverage within a 200 NM radius of Perth is also required. ISASI 2004, Campbell, Flight Data Analysis 2

A transponder-equipped aircraft is not always detected by secondary radar. This could be due to one of the following reasons: 2.2 Accuracies aircraft is outside of the range of the radar transponder is not switched on transponder is unserviceable loss of aircraft power to the transponder terrain shielding aircraft transponder aerial is shielded from the radar due to aircraft manoeuvring The radar rotates at 16.2 RPM giving a scan rate of 3.7 seconds. The accuracy of the radar position data is proportional to the range of the aircraft from the radar site. Typical accuracies for a monopulse SSR are: Range Accuracy : ± 0.05 NM RMS Azimuth Accuracy : ± 0.05 RMS The overall accuracy can be affected by terrain or meteorological conditions. The Mode C Pressure Altitude data accuracy is determined by the aircraft s encoding altimeter accuracy plus the transponder quantisation of 100 feet. An encoding altimeter can suffer from lag when experiencing high vertical speed changes. 3. ECU DATA 3.1 Background The Bell 407 was fitted with a Rolls Royce 250-C47B turbine engine. The ECU is a component of the engine Full Authority Digital Electronic Control (FADEC) system. The ECU was located forward of the main rotor transmission (refer to Figure 1). The ECU has a non-volatile memory (NVM) that can store engine and other parameters. When it detects an exceedance it functions as an incident recorder and is designed to store 60 seconds of data commencing 12 seconds prior to the start of the exceedance. ISASI 2004, Campbell, Flight Data Analysis 3

3.2 Parameters The following parameters were recorded: Mnemonic: Name: Units: Timestamp Cumulative Engine Run-time hhh:mm:ss.sss Nr Rotor Speed % Ng (N 1 ) Gas Generator Speed % Np (N 2 ) Power Turbine Speed % MGT Measured Gas Temperature F Q Torque % Wf Fuel Flow pph NDOT Rate of change of Ng %Ng/sec P1 Ambient Pressure psi Mode Engine Control Mode (Automatic/Manual) 1=Auto CP Collective Pitch % PLA Power Lever Angle Degrees T1 Compressor Inlet Temperature F Each parameter was sampled twenty-two times covering a period of 25.2 seconds. 3.3 Sampling Rate Each parameter was sampled every 1.2 seconds. When an exceedance occurred an additional sample of each parameter was recorded. 4. TIMING OVERLAP Radar data is time-stamped with UTC which is synchronized with UTC obtained from GPS. ECU data is time-stamped with elapsed time relative to the initiating exceedance. As these two time sources were not synchronized it was necessary to determine by other means whether an overlap of the two data sets had occurred. The following observations were made from the radar data: The final radar return was recorded at 1144:45 UTC at an altitude of 2,700 feet (Mode C). The latitude and longitude of the final radar return was located very near the crash site (within 0.1 NM). The final series of returns indicated that a substantial speed had developed. The initial loss of returns was probably due to terrain shielding. ISASI 2004, Campbell, Flight Data Analysis 4

The helicopter subsequently did not climb high enough for radar returns to again be received. The following observations were made from the ECU data: The recording of ECU data ceased when impact occurred. The ECU stored data from the last 25 seconds of flight. Data latency was small as the engine data recorded by the ECU was directly available and not transmitted by other systems. Considering the above observations it was considered highly likely that the radar data and ECU data did overlap in time and that the manoeuvre leading to the development of the substantial speed, initially captured by radar, was the same manoeuvre subsequently captured by the ECU. Pressure altitude was the only common parameter and it was used to try and correlate in time the two data streams. 5. PRESSURE ALTITUDE 5.1 Radar Mode C Pressure Altitude Pressure Altitude referenced to 1013.2 hpa was recorded with a resolution of 100 feet. The source of the pressure altitude was an altitude encoder in the helicopter. A static source provided static pressure to the encoder. Mode C pressure altitude is monitored by ATC and in comparison with the altitude derived from the ECU it was considered to be accurate but limited by resolution. Refer to Figure 2. As the reported QNH was 1014 hpa approximately 30 feet needed to be added to the recorded Mode C values to give pressure altitude referenced to QNH. 5.2 ECU Ambient Pressure The ECU recorded ambient pressure which was used for fuel scheduling purposes. It was sourced from an open port on the ECU itself. The port was not connected to a static pressure line. Given its location it was susceptible to pressure fluctuations due to airflow from the main rotor. Ambient pressure is an accurate indicator of pressure altitude as long as certain assumptions are met. One assumption is that an accurate source of static pressure is available and if so standard conversions can be used to convert pressure to altitude. This assumption was not satisfied for the ambient pressure data recorded by the ECU and corrections needed to be applied to convert it to pressure altitude. Refer to Figure 3. ISASI 2004, Campbell, Flight Data Analysis 5

5.3 ECU Pressure Altitude Offset The highest Mode C pressure altitude recorded was 3,700 feet and the highest pressure altitude obtained from the ECU was 4,370 feet. This indicated that the ECU was over-reading by at least 670 feet. The final pressure altitude obtained from the ECU was 870 feet. Given the small data latency expected for the ECU then this value was the approximate sea-level value allowing for the sampling interval of 1.2 seconds. 6. TIMING CORRELATION Overlaying the Mode C and ECU pressure altitude traces showed that a good match was obtained when the ECU altitude was offset by -850 feet and the end of the Mode C trace was overlapped by the start of the ECU trace. The duration of the overlap was approximately 11 seconds. The tolerance of the duration of the overlap is considered to be ± 2 seconds. Refer to Figure 4. 7. ANIMATION OF THE ECU DATA While computer animation is recognised as being a very useful means of assimilating large quantities of information it is also very useful when analysing limited data sets such as the ECU parameters. The ECU data was imported by the ATSB s Hewlett Packard C3000 computer for presentation using RAPS version 5.0 software. A simulated instrument panel was developed to display key parameters in real-time. Refer to Figure 5. While the ECU sampling interval was 1.2 seconds the frame rate of the animation was much higher eg. 100 frames/sec. Intermediate values were linearly interpolated. Torque Instrument: The pointer and digital display were directly driven by the ECU torque data. MGT Instrument: After the values in degrees Fahrenheit were converted to degrees Celsius, the pointer and digital display were directly driven by the ECU MGT data. Ng Instrument: The pointer and digital display were directly driven by the Ng data. ISASI 2004, Campbell, Flight Data Analysis 6

Collective Display: The pointer and digital display were directly driven by the collective data. Rolls- Royce advised that maximum collective corresponded to a recorded value of approximately 60%. Nr/Np % RPM Instrument: The pointer and digital display were directly driven by the Nr/Np data. Time: A time counter in seconds with the zero datum at the end of the ECU recording ie. at the time of impact with the water. A value of 25.2 corresponds to the start of the ECU data. Altimeter: The ECU ambient pressure data (psi) was converted to pressure altitude. The pressure altitude was smoothed and used to drive the display. Vertical Speed Indicator: Derived from the rate of change of pressure altitude. The animation was very useful in showing the correlation between parameters eg. the relationship between Nr/Ng due to governing. These relationships are not always evident from a data listing. It also put the data into time perspective. 8. CONCLUSIONS Non-FDR data is becoming increasingly available from accidents involving general aviation aircraft and smaller helicopters. While these aircraft do not require an FDR they are often fitted with avionics which can store data. Analysis of this data can be very useful to an investigation. Computer animation of these limited data sets can provide valuable information that is not readily apparent from a data listing. Data obtained from sources other than the FDR may be inaccurate and uncalibrated and require careful analysis. ISASI 2004, Campbell, Flight Data Analysis 7

Figure 1 (1) (1) Sourced from Service Bulletin 407-99-31 Bell Helicopter Textron. ISASI 2004, Campbell, Flight Data Analysis 8

Radar Mode C Altitude 40 35 30 25 Feet*100 20 15 10 5 0 11:43:50 11:43:54 11:43:57 11:44:01 11:44:05 11:44:08 11:44:12 11:44:16 11:44:20 11:44:23 11:44:27 11:44:31 11:44:34 11:44:38 11:44:42 11:44:45 UTC (hh:mm:ss) Figure 2 ISASI 2004, Campbell, Flight Data Analysis 9

ECU Derived Altitude 5000 4500 4000 3500 3000 Feet 2500 2000 1500 1000 500 0 0 1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 16 17 18 19 20 21 22 23 24 25 26 Elapsed Time (seconds) Figure 3 ISASI 2004, Campbell, Flight Data Analysis 10

Combined Mode C and EEC Altitudes 4000 3500 3000 2500 Feet 2000 1500 1000 500 0 Time Figure 4 ISASI 2004, Campbell, Flight Data Analysis 11

Figure 5 ISASI 2004, Campbell, Flight Data Analysis 12