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…
Temperature effects were discussed previously in 'this report.
Those discussions on superheat end adiabatic temperature change
will apply to the general equation. In general, temperature of
the free air and lifting gas can be measured to a fair degree of
accuracy.
Balloon volume at any time is a function of original full balloon
volume plus the summation of all the changes in volume due to pres-
sure and temperature changes and loss of lifting gas. It will
also be affected by loss or gain of: air by the balloon through
diffusion and intake of air through the appendix. The non-
extensible balloon will have a maximum volume and thus any changes
tending to increase the gas volume to a value greater than the
balloon volume will result in a valving of the excess lifting gas
into the air, or {in "the ease of a balloon which will carry in-
ternal pressure) a pressure increase of the lifting gas.
It is for this reason that a non-extensible balloon is said to be
in a state of stable equilibrium in a direction of greater e.l ti-
tude When it is full. Eowever, in a direction of lesser altitude,
and with the case of a p:lrtially full floating balloon, the syste!!_l
is in a state of neutral equilibrium.
Composition of the lifting gas will change due to contamination of
the lifting gas by the entry·of air into the balloon, either by the
flaw of air through thE> appendix opening or by diffusion of e.ir into
the balloon. We may then modify our term for density of the lifting
gas to include a term for the pure gas and a term for the contaminating
air. Using the method of pertial volumes, we me.y equate the density
of the lifting gas at any time by:
p = Pg ( ~ + :iJL )
where: g VbT g Rp Ra
Pg = pressure of the lifting gas
vb • total lifting gas volume
Vp = volume of pure lifting gas in balloon
Va = volume of air in balloon
Rg = epecific gas constant of pure lifting gas
R0 = specific gas constant of air
Then , calling (here we see that since
we may equate:
....!1(-!JL ... _!g_)Tg Rp R0
-59-

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.