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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…
sufficiently to caaae.a Short between the electrodes, firing the squib
prematurely. If the distance is too large, however, therewill be too
great a height difference between the ttme of minimum pressure and the
time the electrodes are shorted. For instance, a spacing of 10 l!Uile would
delay the firing of the squib until the pressure reached 13.3 mb. above
the min~um pressure. At an altitude of 50,000 teet, the equivalent height
(standard atmosphere) would be about 2300 feet. It is obvious that tor high
level flights, a less dense rund lower freezing electrolyte tor the minimum
pressure gwitch ~11 be needed to obtain the desired sensitivity of 2000
teet.
By adding the pressure-activated automatic ballast valve to the
manual ballast valve, the complete patter.n of the solid curte in Figure 7
may be achieved ideally. At sunset the rapid cooling oaases descent which
cannot be canpensated for by the manual ballast valve. As soon as the seal-
off pressure of the automatic ballast valve is exceeded by the atmospheric
pressure, ballast flow is begun, Which restores the balloon to its ceiling.
The dashed curve in Figure 7 shows the action of a balloon when the
automatic ballast valve alone is used tor control purposes. In this case
the balloon ~11 si:rlk slowly from its ceiling (where full buoyancy just
equals the load) to the level where the e.utom tic ballast valve drops
ballast at a rate equal to the diffusion (the floor). It will be noted
that a flight which is controlled in this manner is less wasteful of
ballast and results in a correspondingly longer flight. lne "floor"
determined by this valve varies diurnally as the temperature (hence pressure)
of the air entrap}?ed in the diaphragm is affected by solar radiation. 'i'le
amplitude of this diurnal oscillation may be as much as 6000 feet. the nignt
level being higher than the day level.
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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.