6 Oct 1967 - Vandenberg AFB, California, USA
6 October 1967 19:00
Vandenberg AFB, California, USA

Radar returns and a scintillating object

An unidentified object was tracked by radar and sighted visually.

Condon Report: Case 35. Vandenberg AFB, Lompoc, Calif., 6-7 October 1967, 1900-0130 LST. Weather: clear, good visibility, strong temperature inversions near the surface caused by advection of very warm (80°-90°F), dry air over the cool ocean surface (water temperature 58°-59°F). This sighting begins with an apparent mirage (of a ship probably 60 mi. beyond the normal horizon) and continues with a very large number of unknown targets that were found on tracking radars which were being used in a search mode (they normally are not used in this way). The project case file contains a good analysis of the probable nature of the radar targets, some of which were apparently birds and some apparently ships tracked at 80 mi. ranges as well as other AP-like returns that may have been associated with local intensification of the ducting layer. The nature of the visual objects is not as clear, although at least two of them appear to have been superior mirages of ships beyond the normal horizon. There were possibly some meteor sightings involved.

The meteorological conditions were quite interesting. The warm, dry air was apparently quite close to the water surface, at least in places. Data from Vandenberg and San Nicholas island indicate that in places the inversion was no thicker than about 90 m. (10 mb pressure difference). The contrast that may have existed can be calculated from these data:

  • At or Near Sea Surface: / At 90 Meters or Less:
  • Pressure: / 1004 mb / 994 mb
  • Temperature: °F: / 58°F / 90°F
  • Temperature: °C: / 14°C / 32°C
  • Temperature: °K: / 287°K / 305°K
  • Optical N (5570A) / 275 (ppm) / 256 (ppm)
The optical refractive index gradient that may have existed at the time was therefore on the order of -210 ppm. km-1, or a somewhat greater negative value, depending upon the thickness chosen for the layer. The value above is computed as (256-275) /0.090, based on the 90 m. maximum thickness assumed. Since the critical value of the gradient for a superior mirage is -157 ppm. km-1, it is quite apparent that the conditions required for the formation of extended superior mirages were most likely present on the date in question. The only problem with this explanation is the reported elevation angle of 10°, but as pointed out in the conclusions to this chapter such estimates by visual observers are invariably over-estimated by a large factor. In summary, the conclusions arrived at by the investigators in this case seem to be adequately supported by the meteorological data available.

The sighting reported for 12 October 1967, 0025 LST, seems to be a classic example of the description of a scintillating, wandering star image seen through a strong inversion layer. Note particularly the estimated ratio of vertical and horizontal movements. Two very bright stars would have been close to the horizon at this time: Altair, magnitude 0.9, would have been at 277° azimuth and about 4° elevation angle; Vega, magnitude 0.1, would have been at about 313° azimuth and about 12° elevation angle. Of the two, Altair seems the more likely target because of the smaller elevation angle; the observers gave no estimate of either azimuth or elevation angle.


Hynek rating: RV: Radar-Visual UFO reports
Vallee rating: MA2: MA1 plus any physical effects caused by the UFO.
Other sightings in this area

Google map of this location.


Sources: 813  
 
 
 
 
 
 
 
 

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