In post number 1751 on this thread, Tom Kaye presented radiosonde data for Salem, Oregon (which is about 45 Nautical Miles south of Portland International Airport) and a location that is northwest of Seattle (more than 120 Nautical Miles from Portland International Airport). Unfortunately, some of this data appears to have been affected due to a malfunction of the radiosonde equipment.
Consequently, some judgment was needed in interpreting the radiosonde data. But after all things were considered, the wind direction was essentially from 225 degrees from 4000 feet to 10,000 feet and the wind speed varied between 31 and 35 knots (Nautical Miles Per Hour) over that same range. These supposedly accurate wind speeds are somewhat greater than the predicted winds aloft speeds for the Portland area for the same time frame that is of interest here. However, the wind speed of 31 knots from 225 degrees at 10,000 feet agrees quite well with the 32 knots from 215 degrees that I had arrived at during the flight path analysis for that altitude.
For the present analysis, four altitude segments were used and the time for the placard to descend through each of those segments was calculated and used to determine the horizontal distance that the placard traveled during those times. The horizontal distances were summed and totaled 6.8 Nautical Miles. This places the separation point for the placard about 1.3 Nautical Miles WEST of a straight line between the Malay and Canby Intersections. Earlier calculations using estimate data placed the separation point about 1.0 nautical miles EAST of a straight line between the Malay and Canby Intersections.
In the initial placard calculations in 2011, Tom Kaye suggested evaluating the influence that rain would have on the descent of the placard. There is no information on any weather above the 5000 foot overcast. But there were light rain showers in the Portland area. Surprisingly, there is quite a bit of information on the internet about the influence of rain on falling objects. At one end of the scale, large rain drops would increase the rate of descent. At the other end of the scale, light or misty rainfall would slow the rate of descent. Since the available weather information indicated only light rain below 5000 feet, the rainfall effects were ignored and were conservative in any event.
The end result of the placard analysis is that it separated at a point that was close to, either EAST or WEST of, a straight line between the Malay and Canby Intersections. And that straight line passes about 1000 feet to the WEST of the money find location at Tina Bar.
While there was light rain and several cloud layers including a complete overcast at 5000 feet in the Portland area, the weather was reasonably good and improving as indicated by the sea level pressure being above standard and increasing at all points south of Seattle. In addition, the air temperatures were below standard and the overall result was that the atmospheric density in the Portland area was about two percent above the standard density.