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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…
We may use this equation to approximate the rise of a full balloon system when controlled by overcompensated constant ballast flow:

$$
\frac {d z}{d t} = \frac {d W}{d t} \times A
$$

where z is the balloon ceiling, t is time, and W is total weight of the balloon system.

## B. Rate of Rise

The equation of Clarke and Korff:

$$
\frac {d z}{d t} = 2 7 2 \frac {F ^ {1 / 2}}{G ^ {1 / 3}} \frac {c m}{s e c}
$$

has been used to obtain the relationship between rate of rise and free lift (or excess buoyancy) for a balloon system of any given weight. For practical use, the equation has been modified to:

$$
\frac {d z}{d t} = 1 4 8 6 \frac {F ^ {1 / 2}}{G ^ {1 / 3}}
$$

where F is free lift in pounds and G is gross lift in pounds.

Although this equation was derived for use with extensible spherical balloons, it predicts closely the performance of non-extensible balloons while they are rising to floating level. An average value for the constant in equation (2) from actual flights is 1600 ft./min(1b.) $ ^{1/6} $

The deviation from this relationship, evidenced in several flights, may be due to several variations from the assumptions upon which the equation is based. This deviation has in general been an increase of rate of rise of from 0 to 25% at higher altitudes.

To explain this increase, let us first investigate the changes which may occur in the free lift. If any gas leaves the balloon because of leakage through the balloon or the appendix, the free lift will be reduced and the rate of rise will decrease (as it does after the balloon is full and "levels off"). Therefore, this variation may be ruled out when considering rise before the balloon becomes full.

Free lift will vary with changes of temperature of the lifting gas with respect to the free-air temperature. A change of this sort can be caused by acquisition of superheat of the lifting gas, or by temperature decrease or increase caused by adiabatic expansion or compression of the lifting gas. (These items will be discussed later in this report.) Actual temperature measurements during rising portions of flights indicate that there is no appreciable tempera-

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