I'm posting a comment made by Hominid back in 2011. it's about the weather, and the flight path. It's good information that I need in my testing......Hominid hasn't logged in for a long time? I'm a little concerned about him. I'll email him and see if he is ok. his last login was January 12, 2015
There have been some claims that the weather was very bad as Flight 305 came through the Vancouver-Portland area. Some of this has been in relation to someone in a helicopter at unspecified locations and times, but at 2500'. Some has been about the Columbia River Gorge (which extends many miles to the east along the river starting a few miles east of Portland and Vancouver, and is basically the border between Oregon and Washington in that area).
The claims are inconsistent with NWS data that has been reproduced at WeatherUnderground.com, but the weather data FBI agent Carr posted (then, Georger reposted) provides an opportunity to check about the claims using data that was actually produced by the predecesor to the National Weather Service on that night. The data includes reports of weather conditions for Portland International Airport (PDX), Troutdale airport, Toledo airport and The Dalles at 8pm (image 6b), 9pm (image 5b) and 9:17pm (part 1 of image 1b) PST. Troutdale is a little east of PDX practically at the mouth of the gorge. The Dalles is further east, actually in the gorge. Toledo is a few minutes north of the Vancouver plain.
PORTLAND AIRPORT
The maximum cloud coverage ("overcast") was at a base of 5000' for all three observations, from 8pm through 9:17pm. Over that time frame, the "broken" layer base rose from 2700' to 3100' to 3500' (all AGL). In other words, the layer that (with any lower layer) provided over .5 coverage was rising over the period. The sky was clearing below 3500' and a helo at 2500' AGL would have been below most of the cloud coverage the entire time.
Over that same time sequence, an 8pm "scattered" layer at 1500' AGL was gone at 9pm, but was then back at 9:17. In place of that scattered layer, a few "CUFRA" at 1500' were reported at the intermediate time (when the scattered layer had disappeared). I believe from this that the CUFRA was the remains of the scattered layer of clouds rather than clouds that were ripped away from larger clouds by winds, or formed by the higher clouds. That is, the scattered clouds had shrunk to almost nothing and were identified as CUFRA because of their appearance. A 2500' helo would be above this base in clear air or scattered clouds.
Also, the horizontal visibility (air "clear-ness") peaked at the intermediate observation time. It was 7 statute miles (SM) at 8pm, went up to 10SM at 9pm (when the low clouds were disappearing), then went back to 6SM at 9:17. Light showers were reported at each time.
The existence of the data for 8pm and 9pm in the data Carr posted gives us an opportunity to fill in between the 7pm and 10pm data from WeatherUnderground. Combining data from the sources shows that the wind speed went from 4.6mph at 7pm, to 11.5mph at 8pm, to 12.67mph at 9pm, to 11.5mph at 10pm. The wind speed went abruptly up from nearly dead calm between 7pm and 8pm, then stayed approximately constant for the next two hours.
Similarly, the wind direction changed from 130° (SE) at 7pm (when there was barely any wind) to 270° (W) at 8pm to 190° (S) at 9pm and to 200° (SSW) at 10pm. The abrupt change of the wind to west at 8pm, then back to SSW at 9pm is intriguing. (BTW: wind directions are plus or minus 5°.)
Note how some possibly significant transient weather data is missed by WeatherUnderground because of their giving data for only every third hour.
The wind direction for 7pm is basically meaningless because of the fact that the wind speed was so low. Winds often change direction frequently and erratically when their speeds are low. This is partly because the small perterbations in various directions are what remain when the sustained wind drops to near zero. The low wind has no "conviction." It's "indecisive."
Other than the 8pm west wind, I do not see change much different than the changes for earlier and later days. If you're looking at the WeatherUnderground page for PDX on 11/24/71, you can select to view data for the entire week at the top of the data table.)(Also see attached.)
However, the virtual dead calm from 4pm to 7pm is not present for days shortly before or after the 24th. What does that calm, followed by the abruptly higher speed and short-term west wind, imply for weather near Portland in the following hour? It looks like the 3 hours of calm was a calm before a weak windstorm, not a "calm before THE storm." But it may have just been a random situation of two 3-hourly observations in a row being the same.
TROUTDALE AIRPORT
From 8pm to 9pm to 9:17pm the base of the sky obscuring (overcast) cloud layer rose from 4000' to 6000' AGL. At 8pm no lower layer was reported. At 9pm a layer of "broken" clouds (over .5 coverage) developed at a little under 2200' AGL. It rose to 4000' AGL at 9:17, at which time a "scattered" layer had developed at 1500', the horizontal visibility had dropped to 7SM (from 10), and the wind direction had changed from 220° (SSW) to 270° (W). (wind directions ±5°) Over the period, wind speed had gone from 7kt to 21kt/24mph (9pm) to 12kt. Light showers at 8pm, very light at 9pm, and back to light at 9:17pm.
In general, showers and vertical visibility diminished and wind increased for the intermediate observation. Then the wind direction changed and the horizontal visibility dropped a bit. The cloud cover heights increased, but a lower coverage layer appeared. A 2500' helo could have been above a cloud base at any time after 8pm.
Generally mild weather at the mouth of the gorge, but the wind did pick up a bit after 8pm.
THE DALLES
Much of the info for 8pm (just below the line for Yakima "YKM") is illegible in the 8pm report. It appears that the wind was 9kt from 200°.
At 9pm there was a "scattered" cloud layer at 1500' and a "broken" layer at an estimated 6000' (AGL). Visibility was 15SM. 6kt wind from 310°. No precipitation was reported for 9pm, rain having begun at 8:04 and ended at 8:06 (2 minutes of rain).
At 9:17pm the scattered layer had risen to 2500' and the broken layer had fallen to 4000'. Light showers, wind 15kt (17mph) from 270° (W). The 9:17 report included "chance of light XC" (whatever that meant).
For the entire day, the WeatherUnderground site indicates that The Dalles got only .08" of rain.
In general, wind dropped and changed direction a bit at 9pm then went back some at 9:17. Cloud layer heights changed.
Mild weather at this point in the gorge, except that the wind did go up a bit at 9:17.
TOLEDO
Toledo was not on the 9:17 report in image 1b, as far as I could tell. At 8pm its report said 3000' AGL overcast (complete cover), 12SM visibility, very light showers, 5kt from 190°, and rain had begun at 7:35. At 9pm the report was 3000' scattered, 3400' measured ceiling/overcast, the same visibility, no rain, 6kt (virtually the same) from the same 190°, and rain had ended at 8:05.
Very mild conditions at both 8pm and 9pm a few miles north of Vancouver. A 2500' helo would have been under the cloud base.