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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.
“Sea”26 pages
- 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…
to activate the ballast valve. A fixed ballast leak of about 400 graas
per hour was caused' by a defective valve fitting and this was suttialent
to maintain the balloon at nearly constant level until all the ballast was
exhausted. Following this experience, the use ot a preset fixed leak was
employed on many flights.
The very unstable "floating" seen on Flight 10, when the automatic
ballast valve controlled the flight. is not found on this flight Where the
vehicle used only a fixed-leak control. This eliminates both the over-
compensation and the serious effects ot temperature changes on the aneroid
capsule,. which are found when the automatic ballast valve is used.
The trajectory ot this balloon (Figure 8) shows a very interesting de-
formation at the transit ot the Sacramento Mountains. The anti-cyolonic
Figure 8
curvature over the eastern slope suggests that the air stream at the floating
level was distributed by the terrain. and the deformation predicted by d~c
theory may thus be given a physical illustration. The trajectory was de-
termined by aircraft and theodolite qbservation.
Another striking feature of the flight is the disagreement between the
actual flight path and the trajectory which might have been estimated tram
routine upper-wind reports. Reports from .l!il Paso, Roswell. Albuquerque and
White Sands were used for comparison with the observed trajectory.. Except
tor White Sands, none of these stations reported any wind from the WSW at or
near the floating level during the 12-hour period cqvered by the flight. At
White Sands a very shallow current was detected moving in the direction indicated
by the balloon flight. This clearly demonstrates the non-representiveness ot
the ord~nary pilot balloon observation.
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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.