gismo
Touchdown! Greaser!
Lance,
Not sure where you are getting that the report only lasted one minute. In the remarks it says that freezing rain BEGAN at 58 minutes after the hour and snow ENDED at 58 minutes past the hour.
Although, I do think that the FZRA report might have been incorrect. I dug up a report from another site that was a "corrected" report at 0505 UTC that did not include FZRA.
KBUF 130505Z COR 25012KT 4SM -SN BR BKN008 BKN015 OVC021 01/00 A2983 RMK AO2 CIG 005V011
I'm pretty certain I saw a METAR from BUF that indicated a pair of began and ended times that were one minute apart e.g begin 47 end 48. I would also assume that an identical begin/end pair would indicate equal to or less than 1 minute of precip, is that correct? Seems like for an hour duration, the begin and end times would be in different METARs.
Based on my look, they descended out of 16,000 feet into IMC about 11,000 feet (and that seems to be supported by the CVR and cloud top temperatures on the IR satellite). They would remain in conditions that still had a considerable probability of supercooled liquid water through the point of descending on the ILS approach. If so, they could have accreted a good bit of ice in that time period, especially if there were spotty areas of freezing rain or freezing drizzle aloft. They were on the edge of some heavier precipitation that had 25 - 30 dBZ refectivity. Moreover the BUF 0000 UTC RAOB clearly exhibits a temperature inversion between 5,000 and 6,000 feet that can increase the drop sizes as are discussed in my training programs.
That mostly makes sense to me but if the tops were around 11000 MSL (that was my take as well from both the Skew-T and the ATC transcript) how could there be any freezing rain at or slightly below 11000? Seems like you'd need a vertical extent well above that to generate rain at that altitude. And it's my contention (albeit not necessarily a given) that once they started down from within the cloud layer tops they would have been in a pretty much continuous descent which should mean that they'd be through any layers of SLD rather quickly. IIRC both the Roselawn and the DTW incidents involved flying at a constant altitude for an extended period in the SLD, and in the case of Roselawn they were actually holding and thus making repeated passes through the worst of it. A common method of dealing with icing is penetrating with a rapid descent, I hope this is a valid strategy.
And that's the issue, runback or drops that penetrate the boundary layer behind the protected surfaces which is common in SLD scenarios. You can't shed this ice and it then becomes an efficient ice collector.
Understood. If the flight experienced that they were indeed in serious trouble the moment ice started to accrue behind the boots. And I would think that since the crew had noticed ice on the wings, they would have also noticed if it was building behind the boots and would have been aware of the significance of that. I sure know that would get my full attention as soon as my heart began beating again if I ever saw that happening to my wings.
BTW, here is a very good report just to the west of Buffalo of light to moderate rime from 3,000 to 6,000 feet.
YZ UA /OV CYHM 090035 /TM 0334 /FLDURD /TP C208 /IC LGT-MDT RIME 030-060 /RM TEMP A030 -4, A060 -10
I have no doubt that icing conditions existed, I'm still surprised that it was severe enough to down that plane if it's deice systems were operating as designed. Hopefully a more detailed transcript of the CVR will shed some light on whether or not ice was building behind the boots due to runback.
One other part of the reports so far that I think is a bit puzzling is that the FDR logged significant excursions in pitch and roll which doesn't seem consistent with a tailplane stall, but it would make sense if the upper surfaces of the wings were severely contaminated as well as the tail.