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The Roswell Report: Fact vs. Fiction in the New Mexico Desert

USAF / The Black Vault · 1995 · 882 pages · text by OCR

The Roswell Report: Fact versus Fiction in the New Mexico Desert was published by Headquarters United States Air Force in 1995. The Black Vault distributes this copy. It reproduces the report by Col. Richard L. Weaver and the synopsis by 1st Lt. James McAndrew, both written after a General Accounting Office inquiry requested by Representative Steven Schiff. The Air Force search found no evidence of an extraterrestrial craft or crew. It concluded that the Roswell debris most likely came from NYU Flight No. 4, a Project MOGUL balloon train.

  • p. 193 …overhead and followed the balloons out to sea. I have no idea about the results that…
  • p. 200 …the regular 334 that we had at sea level. From that they could deduce the temperature…
  • p. 243 …actually located on the jurisdictional lines between Sea Girt and Springlake, New Jersey. It was an…
  • p. 244 …The Sea Girt Inn? A: Exactly. That's where John had his office, and I was…
  • p. 320 …alone is about 24,000 miles at sea level, and about 4500 miles at 45,000…
  • p. 325 …twenty-five (25) feet at their largest sea-level diameter. The sonic unit was a combination…
  • p. 378 …per hour when one-fifth inflated at sea level). One other type of balloon which has…
  • p. 402 …Let us, then, compare the rate of leakage at any given altitude with leakage at sea…
  • p. 404 …The leakage at any altitude may be expressed as a function of leakage at sea level…
  • p. 405 Comparing rate of leakage at 40,000 feet with leakage at sea level: $$ \frac {L _ {4…
  • p. 407 …If a 20-foot diameter balloon $ \frac{1}{1 0} $ full were tested at sea level…
  • p. 408 …At sea level this is equivalent to 5.32 gm/hr. for a 20-foot diameter…
  • p. 414 …Using the rules of subsonic aerodynamics, Picard suggests that air at sea level escaping at 1333…
  • p. 415 …air at sea level (lb./ft. $ ^{3} $ ) 14.7 = pressure of air at sea level (psi…
  • p. 432 …to about 20 millibars and increased to sea-level pressure at different temperatures. The most comprehensive…
  • p. 563 …The height above mean sea level as determined from pressure measurements used in this work with…
  • p. 644 …point at which the radiosonde reaches the sea surface. ## 2. Earlier attempts There have been numerous…
  • p. 645 …The balloons floated between the surface and 30,000 ft above sea level; those which reached…
  • p. 704 …Met Gifford who has 90' sea rescue boat this project is planning to use. Stayed at…
  • p. 719 …Worzel working on gravity at sea. Saw Geo Woollard and the Ryders. Woollard after Guggenheim fellowship…
  • p. 779 …the launching site is markedly different from sea level, a shift in this curve is needed…
  • p. 817 …balloon at all times with respect to sea level. On this curve also it is customary…
  • p. 825 …The height above mean sea level as determined from pressure measurements used in this work with…
given point in a cross-section through the atmosphere was misleading.

In order to avoid the suggestion of greater precision than was warranted by the character of the information available, it 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 conditions existing during experiments being conducted 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 project, 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 wind conditions at the 200 mb level of the atmosphere. Flights were to remain afloat until they had traveled approximately 1000 miles.

In order to track the balloon systems, the AM-1 transmitter 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 brush 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

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Report, cited by the archive. The PDF is mirrored here; the original link is under it. The text was read from the page images by an OCR model; expect the odd misread word. 882 pages are in the text index: search them above, or from the library's search.