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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…
When the contact is made, the load line is cut and the entire weight of the dependent equipment is used to pull out a section of the balloon wall. Through this rupture, the lifting gas can escape, and the balloon descends, using the upper portion as a parachute. The rate of descent has been observed to vary from 600 to 1500 feet per minute when this system is employed.

For some special applications it has been desirable to cause the balloon to descend after some predetermined time, instead of waiting for the descent to air traffic lanes. In these cases, a clockwork switch has been used instead of the pressure-activation unit. When clocks are used they are kept free of lubricants which will freeze. The best results have been obtained from the use of a Dow Corning Silicone (DC 701) diluted with 30% kerosene. If this is not available, it is better to send up a clock without any lubrication. Given relatively loose mechanism (a cheap alarm clock) the differential expansion of parts which is encountered at low temperatures is apt to cause less trouble than does the congealing of standard lubricants.

## IV. EQUATIONS AND THEORETICAL CONSIDERATIONS

Development of a controlled altitude balloon has led to investigation of many theoretical considerations applicable both directly and indirectly to the description of variables encountered in balloon control. Some of these relationships have been derived directly from standard hydrodynamic or thermodynamic principles; others come from an empirical study of results of laboratory tests and actual balloon flights. In this section we will investigate these theoretical considerations and endeavor to correlate them with actual flight results. A more simple investigation of the equations necessary for the launching and tracking of a controlled altitude balloon is contained in Part II of this report, "Operations."

We shall first consider the relationships which aid in evaluating the elementary characteristics of non-extensible balloon flight and those which are helpful in carrying out inflation and launching operations of such balloons. Next, we shall discuss more complex considerations involved in balloon flights.

## A. Floating Altitude and Altitude Sensitivity

To determine the altitude at which a non-extensible balloon will float we must consider the weight of the balloon system, the volume of the balloon, and the densities of the lifting gas and the air. [If the lifting gas is 98% helium (molecular weight 4.50 lb./lb. mol), the lift of a unit of gas will be 24.4 lb./lb. mol. Similarly, if 98% hydrogen were the lifting gas, the lift would be 26.6 lb./lb. mol.] By using these three basic parameters, we can obtain an expression for the molar volume at which the balloon will float:

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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.