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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…
We may use this equation to approximate the rise of a full balloon
system when controlled by overcompensated constant ballast flow:
(8) .dl: ~-A
dt dt
where z is the balloon ceiling, t is time, and W is total weight
of the balloon system.
B. Rate of Rise
The equation of Clarke and Korff 1
(1) ..dl.:
dt
F'lz
2 em
21 '"IT" secGt3
has been used to obtain the relationship between rate of rise and
free lift ~r excess buoyancy) for a balloon system of any given
weight. For practical use, the equation has been modified to:
(2) d! Fl/z
dt = 1486 GVi where F is free lift in pounds
and G is gross lift in pounds.
Although this equation was derived for use with extensible spherical
balloons~ it predicts closely the performance of non-extensible
balloons while they are risin~ to floating level. An average value
for the constant in equation .{2) from actual flights is 1600 ft./min(lb. )1/6
The deviatioh from this relationship, evidenced in several flights,
may be due to several variations from the assumptions upon which
the equation is based. This deviation has in general been an in-
crease of rate of rise of from 0 to 25% at higher altitudes.
To explain this increase, let us first investigate the changes
which may occur in the free lift. If any gas leaves the balloon
because of leakage through the balloon or the appendix, the free
lift will be reduced and the rate of rise will decrease (as it
does after the balloon is full and "levels orr"). Therefore, this
variation may be ruled out whenconsidering rise before the balloon
becomes full.
Free lift will vary with changea of temperature of the lifting gas
with respect to the free-air temperature. A change of this sort can
be caused by acquisition of superheat of the lifting gas, or by
temperature decrease or increase caused by adiabatic expansion or
OOilfre&sion of the lifting gas. (These items will be discussed later
in this report.) Actual temperature measurements during rising
portions of flights indicate that there is·no appreciable tempera-
-33-

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.