Documents / Report

Scientific Study of Unidentified Flying Objects (the Condon Report, complete, three volumes)

University of Colorado · 1969-01 · 1497 pages · text from the file's own layer

This is the final report of the Scientific Study of Unidentified Flying Objects, conducted by the University of Colorado under Air Force contract F44620-67-C-0035, with Edward U. Condon as scientific director and Daniel S. Gillmor as editor. It was submitted to the National Academy of Sciences on 15 November 1968 for review. The report includes field studies, photographic and radar analyses, case studies, historical chapters and appendices such as the Robertson Panel report and the Twining letter.

must therefore remain speculative in nature. If the UFOs are CO!l- sidered to have been material objects, then they would have had to have shifted positiun some tens of miles in the "two to four" seconds while the pilot was looking down at his instruments. This does not explain why they cOJ.tinue d to appear on the ground radar. The only admissible hypothesis would seem to he that they became invisible as the fighter approached, but this does not account for the fact that they could not be picked up on airborne radar while the aircraft was searching the area. There is one hypothesis that s';,ems to fit all of the observed facts: that the "ragged formation" was actually an inferior mirage (see Section VI,Chapter 4). TIle angular conditions are satisfied: the objects appeared "slightiy helow the level of the aircraft, II and reflections of the sky above the hori zan would :~eem dark when seen projected against the h3zy sky directly over the city. A layer of heated air, trapped temporarily below a cooler layer by a stable vertical wind shear, could produce a wavy interface that would reflect the sky in a few spots. This phenomenon is qUite similar to the familiar road mjrage. Like a road mirage it suddenly disappears when one gets too close and the viewing angle becomes either too large or too small. If the warm air below , the source of which would presumably have been the downtown area af Dctroit, were also considerably moister than the cooler air ahove as is quite probable, then the radio ref~active index would decrease q~ite suddenly across the inter- face. '111 is would tend to produce anomalous propagati 011 r~ffects, incll~ing false echoes, on rodar, and would explain why ground radar could continue tracking the unknowns when the pilot and aL'lJorne radar operator could no longer see them. 'n1(, airborne radar, p('in~ iml1lersed in the layer would probably no:': recoive All e~hoes of any duration other ~han. perhaps, occasional random blips. 226 must therefore remain speculative i.n nature. If the UPOs are COll- sidered to have been material objects, then they would have had to have shifted position some tens of miles in the "two to four" seconds while the pilot was looking dowll at his instruments. This does not explain why they cOJ.tinue d to appear on the ground radar. The only admissible hypothesis would seem to be that they became invisible as the fighter approached, but this does not account for the fact that they could not be picked up on airborne radar while the aircraft was searching the area. There is one hypothesis that s'~em" to fj t all of the observed facts: that the "ragged formation" was actually an inferior mirage (see Section VI, Chapter 4). TIle angular conclitions are satisfied: the objects appeared "slightiy below the level of the aircraft," and reflections of the sky above the hori zon would !'eem dark when seen projected against the h3ZY sky directly over the city. A layer of heated air, trapped temporarily below a cooler layer by a stable vertical wind shear, could produce a wavy interface that would reflect the sky in a few spots. This phenomenon b qUite similar to the familiar road mirage. Like a road mirage it suddenly disappears when one gets too close and the viewing angle becomes either too large or too small. 1£ the Ilarm air below. the source of which would presumably have been the downtown area of Detroit, were also considerably moister than the cooler air ahove as is quite probable, then the radio refractiVe index would decrease q~itc suddenly across the inter- face. 'l1lis would tend to produce anomalous propagation effects, including false echoes, on radar, and would expln.in why ground radar cuuld continue tracking the unknowns when the pilot and aL'iJorne radar operator could no longer 5t'e them. 'nle airhorne radar, pein~ .ilr.l1lcrseu in the laycr would probably no'~ recoive AI' echoes of any duration other ::han, perhaps, occasional random blips. 226

Cases discussed

About this file

Report, from the classic collection. The PDF is mirrored here; the original link is under it. 1497 pages are in the text index: search them above, or from the library's search.