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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…
given point in a cross-section through the atmosphere was
misleatling.
In order to avoid the suggestion of greater precision than was
warranted by·the character of the information available, it
21.
was decided, during the autumn of 1947 to present the meteorological
diagnoses in a different form. Since that time, graphs (in lieu
of cross-sections) have been constructed to show the vertical
distributions of the estimated ranges, that is to say, the estimated
extremes of temperature and wind on the whole or over a part of
the area involved in each experiment.
Since August, 1950, the principal task has been the preparation
of diagnoses of conditiona existing dt1ring experiments being con-
ducted regularly in eastern Colorado, western Nebraska and western
Kansas by the Industrial Research Institute of the University of
Denver. The design of these experiments necessitates a particularly
careful study of the available weather data and the exercise of
a considerable amount of synoptic ·meteorological judgment in the
preparation of the wind and temperature diagnoses.
F. Flights Utilizing the Constant Level Balloon System
After completion of the balloon control and telemetering development
phases of the projec~, the balloon systems were utilized under
Contracts AF 19(122)-45 and AF 28(099)-10, between this University
and the Air Force Cambridge Research Laboratories. A brief review
of these projects is as follows:
1. High Altitude Balloon Trajectory Study (Contract AF 19(122)-45)
Under the terms of this contract the Research Division was
commissioned to launch and track constant level balloon
systems in order to study -:dnd conditions at the 200 mb
level of the atmosphere. Flights were to remain afloat
until they h~d traveled approximately 1000 miles.
In order to track the balloon systems, the AM-1 trans-
mitter was operated at 1746 kc, using the radio compass
from an aircraft to "home in" on the balloon and position
it at specified time intervals. Information on pressure
altitude, ballast flow data and balloon, free air and
transmitter battery pack temperatures was transmitted
through the AM-1 to receivers mounted in the aircraft
and recorded on b~1sh recorders for analysis at New
York University.
A total of 22 flights (two of which crossed the Atlantic
Ocean and were recovered in Norway and Algeria) were

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.