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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…
made on this project. A complete report of these flights
and the egnipment used is included in "Technical Report
121.01 11 ( b J b~r this Research Division.
2. High Neutron Intensity Study (Contract AF 28(099)-10)
In conjunction with a study to determine the altitude of
maximum !leutron density a modi.fication was made on the
Consta.,t AJ.ti t11de balloon system developed under this
contract. In order to study ne,_ttron densities at two
different altitudes with the same set of instruments,
it was desirable to carry these instruments thro•1gh
a "stepped flight". The balloon system in this case
was to asc?nd to a selected altitude (say 45,000 ft.)
float there for one-hour and then ascend to a higher
altitude (for example 65,000 ft.) to float for another
hour before descending.
The advantages of this type .t'light for Cosmic Ray st·~dies
are that a given altitude may be s-anpled for a long
enough period of time to obtain statistically valid
results, and such statistical sampling can be made
at several levels wi tho11t the necessity of releasing .
another balloon system and other set of neutron sensing
instruments. By proper design of equi~ment a fairly
wide range of altitudes can be sampled with "altitude
steps" of almost any desired size.
The step effect is attained by release of a fairly
large amount of ballast at a fast rate set off by a
pre-set clock timer or a radio rele~se activated by
a transmitter on the ground. The amount of ballast
to be released is determined from the standard altitude-
vol•,me load relationships used for constant-level balloon
flight. As a part of the final ballast release, the
ballast tank and its controls may be dropped from the
system.
If the level positions of the flight must be controlled
to fine limits, or if they must be of long duration
(more than two hours) it.is necessary to employ constant-
level ballast control over these portions of the flight.
However, if the level portions of the flight are to be
in the neighborhood of 1 ho~1r duration, ballast control
during the~e floating period~ can be elimin~ted, making
use of the inherent st~bility of the pl::l.stic balloon
systems for short range constant level flights. It is
this latter method which was used by the New York University
gro,p in the study of Neutron Naxima.
22.

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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.