Documents / FOIA release

roswell

Office of the Secretary of Defense · 993 pages · text from the file's own layer

The Roswell Report: Fact versus Fiction in the New Mexico Desert was published in 1995 by Headquarters United States Air Force. It was written in response to Representative Steven H. Schiff's request and a General Accounting Office audit, and it contains Col. Richard L. Weaver's report and 1st Lt. James McAndrew's synopsis, along with attachments, appendices and photographs. The report says researchers found no evidence of an extraterrestrial craft or crew. It concludes that the 1947 debris came from a Project MOGUL balloon train.

  • p. 129 …6099 2 HQ AMC WRIGHT PAT 342-seA-6191 CAMBRIDGE LABS 342-A~ AMC HQ WRIGHT…
  • p. 228 …overhead and followed the balloons out to sea. I have no idea about the results that…
  • p. 235 …the regular 334 that we had at sea level. From that they could deduce the temperature…
  • p. 279 …actually located on the jurisdictional lines between Sea Girt and Springlake, New Jersey. It was an…
  • p. 280 …The Sea Girt Inn? A: Exactly. That's where John had his office, and I was…
  • p. 400 …alone 1a about 24,000.m1lea at sea level, aDd about '500 allea at 45,000…
  • p. 407 …five (25) feet at their ls.rgest sea-level diameter. The sonic unit was a combination…
  • p. 466 …hour when one-fifth inf~ated at sea level). One other type of balloon which has…
  • p. 490 …Let us, then, compare the rate of leakage at any given altitude with leakage at sea…
  • p. 492 …The leakage at any altitude may be expressed as a function of leakage at sea level…
  • p. 493 Comparing rete of leakage at 40,000 feet with leakage at sea level: ~ 188 .u§. - 0…
  • p. 495 …It a 20-foot diameter balloon~ full were tested at 10 sea level and found to…
  • p. 496 …At sea level this is equivalent to 5.32 ~r. for a 20-foot diameter balloon…
  • p. 502 …Using the rules of subsonic aerodynamics, Picard suggests that air at sea level escaping at 1333…
  • p. 503 …sea level (psi) escape velocity of air to produce back pressure of 1 atmosphere at sea…
  • p. 520 …to about 20 millibars and increased to sea-level pressure at different temperatures. The most comprehensive…
  • p. 654 …The height above mean sea level as determined fram pressure measurements used in this work with…
  • p. 686 …to a thtmble a.nd attached to re1n forced pCltches at alterna.te .sea.m.s…
  • p. 688 …lQr9e Ba.lloo n ~hould trQin de .sea nd to 101000'. 6 each.-Gene ral M1lls…
  • p. 736 …point at which the radiosonde reaches the sea surface. 2. Earlier attempts There have been numerous…
  • p. 737 …The balloons floated between the surface and 30,000 ft above sea level; those which reached…
  • p. 801 …Vet Gifford ;.;ho has 0 0' sea rescue boat this project is planning to use. Stayed…
  • p. 816 …Worzel working on gravity at sea. Saw Geo Woollard and the Ryders. Woollard after Guggenheim fellowship…
  • p. 887 …the launching site is markedly different from sea level, a shift in this curve is needed…
  • p. 925 …balloon at all times with respect to sea level. On this curve also it is customary…
  • p. 933 …The height above ~ean sea level as determined from pressure measurements used in this work with…
F~OJECT ABSTTIACTS
Chief: Dr. James A. FeoJ;le.i • ..::::-.
1. Fro.1e:~t tit-le: A.~ol.4s"L: ~ounaing of the Atmcspbe:r-e
f':roject. sdentist.:;: Dr. :. A. i'eople:3, Jr., Dr. i•lor:ua.n
Haskell
Summary cf In-Laborat.:'lry ;·,ork:
'When large explosions i1av-;' o>!curred, it J·.as been observed that the soWla was
heard locally, say up to ::5 mile:s, and als.:> at dbtances of 100 to 200 miles, but
that nothinf; wa:; reard at intermediate distan~es. This phenomeru11can only be
explained by assumjng that the sound ts refracted into ths atmosphere over the 1n-
termedi2te observers and then is bent back down to the ;nore distant areas. For t~ds
to occur t.ho velocity of propagation must first decrease with altitude and then
increase &!&in to a value at least as lar~e a3 ground velocity. this is due to a
decrease of temrerature up t.o the tropopause followed by an increase in temperature
above that level. V:inds also have an appreciable affect which can be determined
from asymmetrical propa~ation.
Up to abo~t 1946 most data on this phenomenon had been obt&ined by taking
polls after accidental eaplosions had occurred. Zones ot audibility were mapped out
and ~ener.al conclusions then drawn. Very lit.tle systematic w·ork was done in \Which
accurate travel tiAs and other factors were obtair.ed. Beginning in 1~46 at these .
laboratories, a systematic study of these pr"p~at!on anomalies were started. Sound~
ran5ing detectors ware set up in arr&Js, so thsarvations h; "te bec!n tG.k6b ih the vicinity of Fairbanl:s• Alaska for in!or.." t on o.t
~.I"i J.igtj latitud~s4 · Ob~er.vatj,.dn,; .ha•e been taken near the Panama Carial Zone for
~:ci~Uiional information i.i1 tbt: !r#i.csi
The sounds produced by rockets launched a\. .k..1ar.togordo have been recol'd~d .~ith
acousti= detector arrays located on the gro1nd neer the rocket trajectory. From data
gath-=red in this nt£11Iler, soraa inoic~ ti.m!:' of apper air te11.par~tl.lre a."lU .viud::> Lo.ve ween
obtained and much :no:e accurate date:rm.im. tion:; could be ;,lade if U1Q rock~t trajectories
were more accurately known.
l

Cases discussed

About this file

FOIA release, from the osd collection. The PDF is mirrored here; the original link is under it. 993 pages are in the text index: search them above, or from the library's search.