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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…
B. Altitude Control Equipment
Flights of 20-foot General Mills balloons, using no con-
trol equipment, have been sent to altitudes of about
50,000 feet. After reaching maximum altitude, the balloons
all exhibit a tendency to float then descend at an in-
creasing rate for periods of from 2 to 6 hours. In stable
layers of air such as the stratosphere the descent of a
ball.o:on is retarded by the helium, on compression, getting
warmer than the surrounding air. This results in much longer
duration flights requiting no external control though,
strictly speaking, the altitude is not constant. This
concept is in good general agreement with the observed
data; balloons have remained in a semi-floating state
much longer ~p to 30 hours) when in the stratospheric
inversion than when in less stable lower atmospheric
layers.
When it is desired to maintain a balloon at constant
level for a guaranteed period of time in excess of two
hours, a ballast system of altitude control should be
added to the flight gear. The level et which the bal-
loon is to float must be the maximum altitude to which
it can carry the payload. To compensate for loss in buoy-
ancy occasioned by loss of lifting gas through diffusion
and leakage, a continual lightening of the load is re-
quired. To effectthis in a simple fashion, liquid ballast
is permittted to flow through an orifice at a predeter.nined
rate which exceeds the expected loss of lift. (See Section
IV, D) The reservoir and ballast assembly which has
been developed for this use is shown in Figure 6. A de-
tail sketch of the orifice in its mounting is shown as
Figure 7, and F'igure 8 shows a suitable filter which
must be used to protect the orifice from clogging. The
liquid ballast must (1) not freeze, but flow well at
cold temperature (-80°C); (2) not absorb water, which
would freeze; and (3) be relatively inexpensive. A re-
commended liquid is Aeromobil Compass Fluid, made by
Socony-Vacuum Co. (Air Force Spec. AN-c-116).
There are three possible objections to the use of this
simple control system. First, a continued lessening of
the total weight on the balloon--with no change in volume--
must result in a constantly rising ceiling. For a 20-
foot balloon et 45,000 feet, this change is approximately
1000 feet with each kilogram of ballast dropped ( see Sec-
tion IV, E). Second, only a prefixed ballast flow is
permitted, and excessive loss of lift, as might come when
the gas is colled at sunset (when the balloon loses superheat:',
-16-

Cases discussed

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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.