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.
“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…
Example: It a 20-foot diameter balloon~ full were tested at
10
sea level and found to have a leakage rate of 50 gmfiu-. the
leakage rate of a full 2D-foot balloon at sea level would be:
Lt • eo;-{1o)f • 34ol
The leakage of a full 70-foot diameter balloon at sea level in
this case would be:
lf • 50 ~ [tof:g}a]f =7820 GII/HR
Values for leakage at several different altitudes for 20-foot
and 7D-foot diameter ballcons, assuming a leakage of 50 ~r.
for a 20-foot balloon~ full at sea level are:
10
.1 titude (MSL) 0 40,000 ft. 100.000 ft.
2o-ft. diam. 340 r. 83.2 r.
70-ft. diam. 7820 r. 1912 r.
Another consideration is that relationship expressed by the
kinetic theory of gases regarding gases at low pressures. The
kinetic theory states that there is a molecular type of flow
across a thin diaphragm through openings whose dimensions are
of the order of the length of the mean free path of the mole-
cules involved. Mass flow of the gas is then:
where:
L = ~p·A~
120
Jl p : 1s the pressure difference across the film
A = area of the opening
dCJ = density of the gas in question
This. relationship, however, becomes valid ot~ly at extremely
low pressures, and when considering balloon systems at no:nr.al
floating levels the more common fluid-flow relationship will
control the rate of loss of lift through openings in the film.
It would be of little use then to investigate further the leak-
age of gas through openings by means of the relationships in-
volved in the kinetic theory.
-46- 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.