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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…
DECEMBER
Year Sur:Cace 1,500 M 3,000 M 5,000 M 10,000 M
El Paso 1944 N-3 NNE-1 W-2 NW-1
1945 NNE-3 W-3 WNW-6 WNW-6
Roswell 1944 S-1 t'W-3 NW-4 V.'NW-6
1945 SSE-3 wsw-2 WNW-5 'WNW-8
Albuquerque 1944 N-3 "WNW-4 WNW-6 W-10
1945 N-3 NW-6 WNW-8 WNW-9
Amarillo 1944 NW-4 NW•4 'WNW-6 WNW-8 'WNW-8
1945 SW-3 W-2 WNW-5 WNW-9
Big Spring 1944 NW-4 NW-5 WNW-6
1945 WSW-3 W-6 VYNW-7 --
D. Tracking Devices: Horizontal
The flights made in the early part of this program were tracked
optically with theodolites. Coupled with the height data, theodolite
readings provide a fairly reliable horizontal locus of the balloon. However,
even in the clear air of New ~xico, this method is useful for not more than
100 miles and, unless accurate height data are available, theodolite stations
provide useful data for not more than 40 miles.
Airora:Ct observations have been used with some success when the ceiling
of the balloon is not too great. It is expected that an inverted AN/APQ-13
radar, mounted atop a B-17, will greatly augment the horizontal tracking
and will be of some value in determining height.
The most useful equipment for determining horizontal movement of the
balloons has been the SCR-658 radio direction finding set. Long after the
vertical angles registered by this gear are questionable (due to reflections
off intervening terrain), the horizontal angles are useable. Used in sets
of two or more, or coupled with height data, these observations give good
position• with distances up to 150 miles. Figure 18 shows the coverage a
network of four of these sets would provide. In contrast to the theodolites
and aircraft ob•servations, these instruments are perfectly operative when
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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.