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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…
decreasing the coefficient of coupling between the primary and secondary of the IF transformers. By this reduction of bandwidth to 3kc a 3 microvolt signal produced a 15.5 DB signal to noise ratio, where at 16 kc bandwidth only 7 DB was obtained.

In order to obtain accurate reproduction of the amplitude of the audio frequency the AVC circuit was modified by adding a fixed bias to the AVC diode of the receiver. This flattened the characteristic of the AVC circuit and no change in amplitude of recorded audio signal was detected over a six hour flight using a constant amplitude audio signal from the transmitter. The signal was tapped off at the output of the second detector of the receiver and fed to a Brush BL 905 AC amplifier for recording. The recorder used was a Brush BL-202 double channel oscillograph. A quarter wave vertical receiving antennae was employed with a counter poise ground. The transmitting antennae was a vertical half wave dipole.

In order to use the AM-1 for transmission of information from pressure and temperature sensors a relaxation oscillator circuit was incorporated in the system. (dotted section - Fig. 6). This oscillator used one half of one of the 3A5 modulator tubes and produced a blocking rate approximately proportional to resistance of the sensor instruments. This information could be superimposed on the regular modulated signal and two types of information could be transmitted simultaneously; one as amplitude and frequency change of the basic signal, the other as a frequency of pulses superimposed on the basic signal.

The AM-1 has been used in balloon control research to transmit information on pressure, temperature and ballast requirements. It was also employed to give information on Neutron intensities in another Air Force project(5). In order to obtain information on balloon position on a wind study project the AM-1 was used as a beacon to be "homed in" on by the radio compass of aircraft(6).

A system of diversity reception was considered for use with a dual channel AM-1 transmitter in order to increase reliability despite atmospheric noise. In the dual channel unit a common modulator was connected to two separate crystal oscillators and RF amplifiers. In preliminary tests two receiver and recording units were used.

For short range balloon flights the AM-1 was modified for use with subminiature and acorn type tubes. In this, the AM-2, two 2E27 tubes in parallel provide excitation for the type 958A RF amplifier. A circuit diagram of this unit is shown as Fig. 7.

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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.