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In-flight upset - 154 km west of Learmonth, WA, 7 October 2008,

In-flight upset - 154 km west of Learmonth, WA, 7 October 2008,

In-flight upset - 154 km west of Learmonth, WA, 7 October 2008,

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etween the values <strong>of</strong> any <strong>of</strong> the four altitude parameters. The FDR recordedstandard altitude, while the QAR recorded standard altitude and baro-correctedaltitude #1. <strong>In</strong> summary, the altitude values that correlated with some data spikescould have originated from any <strong>of</strong> the four altitude parameters.Other parametersA review <strong>of</strong> some <strong>of</strong> the other recorded data did not identify any other salientmatches between the binary values <strong>of</strong> the different ADIRU parameters. However,most <strong>of</strong> the ADIRU parameters were not recorded, and most <strong>of</strong> the data for eachparameter was not recorded. <strong>In</strong> addition, the nature <strong>of</strong> the IR data made it difficultfor the investigation to identify spikes in that data and to establish whether anypatterns existed. As discussed in section 1.11, the IR parameters rapidly divergedfrom realistic values and oscillated between unrealistically large values at varyingrates for the remainder <strong>of</strong> the <strong>flight</strong>.3.3.5 Data-spike patterns for the 27 December <strong>2008</strong> <strong>flight</strong>For the 27 December <strong>2008</strong> occurrence, there was only a 24-second period whenspikes were outputted from ADIRU 1 before the ADR was switched <strong>of</strong>f. Thecomputed airspeed spikes appeared to correlate with altitude data in a similar wayas for 7 <strong>October</strong> <strong>2008</strong> event, but there were too few spikes recorded to form adefinitive conclusion. There were no Mach or AOA spikes recorded. Furtherinformation on the FDR and QAR data are provided in Appendix D.3.3.6 SummaryFor the 7 <strong>October</strong> <strong>2008</strong> occurrence, there was a clear match between the values <strong>of</strong>most <strong>of</strong> the Mach data spikes and the concurrent values for altitude, both at cruiseand during the descent. There was also some evidence <strong>of</strong> data spikes for computedairspeed matching with altitude values in both the 7 <strong>October</strong> <strong>2008</strong> and 27 December<strong>2008</strong> occurrences, and a possible relationship between the AOA spikes and altitudevalues in the 7 <strong>October</strong> <strong>2008</strong> occurrence.The investigation was unable to determine the extent to which other patterns existedin the data spikes because <strong>of</strong> limitations in the recorded data. The investigation wasalso not able to determine whether the repeated values <strong>of</strong> some data spikes were dueto the spike values being stored in memory, or due to the spike values resultingfrom the exchange <strong>of</strong> data with another parameter that did not vary during theperiod <strong>of</strong> interest (such as a documentary data, status data or fault data parameter).3.4 Data flow analyses3.4.1 BackgroundThe investigation examined the LTN-101 ADIRU’s data processing stages todetermine if there were indications <strong>of</strong> which stage or stages problems may haveoccurred. A simplified summary <strong>of</strong> the data flow used for most <strong>of</strong> the output- 121 -

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