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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. 33 …The specific Air Staff/Secretariat offices queried included the following: (a) SAF I AAI, Directorate of…
  • p. 75 …the Public Information Officer, Walter G. Haut, issued a news release that the Amry Air Force…
  • p. 104 …vt. G. Hilburn, f'onner Assistant Base Adj•lba.nt, transferred ~~ Squedr~n "A", 427th AAF…
  • p. 114 …SFERRED A. OfFICE , •. STORAGE A. FILE CABINETS (No.) 1. TRANS. FILES (.Yo.) lc SHELVING (Li•. Fl…
  • p. 133 …reporti.Dc aot later t:t:.a date 1Jl41catecU 8 Jplx 1947 Cl&tl Lt. G…
  • p. 143 …9:15 A.l:. 9:15 A.~. 9:40 li..M. 9:43 A.ll. 9…
  • p. 144 …on fhone requesting a B-29 be sent to Blackstone, Va. for a celebration by the…
  • p. 198 …Cor.anandinr; G~nerel, Army Air Forces, \'/aehint;ton 25, D. C. ATTN s AC/AS…
  • p. 282 …I then went into industry, and I worked for EG&G, a high- technology company based…
  • p. 303 …AlllllffO PAirrS OP rNF ./OSS.tMM:Y WI./.£ FIT AND 01'€/t.ttrl /It A PROYFA…
  • p. 307 …I do not want a lawyer. lamwi · g to answer questions or make a statement or…
  • p. 322 …4 consisted of a "cluster of (meteor(>logi- cal) balloons" and a "regular sonobuoy."23 Presumably…
  • p. 401 …a.:-:1!! of the sound channel would also b~ detectable by l1!te~1r.g at…
  • p. 407 …dribble constructed of a five (5) gallon tin incorporating e 11etered jet to allow a predetermined…
  • p. 418 …O.oJ nnel KN'$~.ll.!a G, ~ftr. 0-18373.. «C •.• _~ .. Retent1Qn: Indefinite. No known replacement…
  • p. 436 …A typical night using constant ballast flow at a rate slightl7 exceeding leakage losses is shown…
  • p. 437 Fig • 9 is a typical night with DO ballaet. !he night train· tor these flights ia…
  • p. 472 …the tloa tin_g level. (The switch is set so that a rate of change ot…
  • p. 483 We may use this equation to approximate the rise of a full balloon system when controlled…
  • p. 488 …A = 2.39 x 108 col I erg Cp = specific heat at constant pressure g = acceleration…
  • p. 490 …flow, Is and a co- efficient of leakage,Cd• (1) where g is the acceleration due…
  • p. 495 …lf • 50 ~ tof:g}af =7820 GII/HR Values for leakage at several different altitudes…
  • p. 506 …tight upon release of this internal pressure. G. A Ge.tleral Equa.ttc:m of Motion…
  • p. 509 …It is for this reason that a non-extensible balloon is said to be in a…
  • p. 510 …a g I -'- (~ .!L) F, = vb Pa LAo To - Tg Rp + Ro Discussions of the contamination…
  • p. 511 …or 9J <{J)G · dt dt lc We might also have a control tbl t will…
  • p. 512 …1t> !!A_} is the- time during which pressure change of the airdlurro8h!1~g the balloon…
  • p. 523 …The performar.ce specifications are as follows: (a) Rotation: one revolution every 12 hours (b) Duration…
  • p. 528 …Adjustments are made on the adjusting screw {L) and the lower ring {G) before each flight…
  • p. 536 …flight, a 65-pound load was lifted with a linear array of 28 350-g~ rubber…
  • p. 553 …On Plight 43 the tiret model ot an Olland-o7cle pressure modulator was tlown with a…
  • p. 558 …and a satisfactory Olland-cycle pressure modulator~& also used .for over 5 hours to give height…
  • p. 560 …This flight was released at night with a fixed ballast flow of about 300 ~rams per…
  • p. 573 …Flight 82 is a good example of i'light using a single fixed-leak orifice for…
  • p. 574 …Below the baroswitoh a standard T-69 radiosonde was supported with a parachute stuffed into a…
  • p. 577 Fli.g!lt 89: Released from Alamogordo, New Mexico, 1005 MST, August 26, 1948 Not recovered…
  • p. 584 …a near-floating condition for about four hours when the transmitter 40 / llllllff-~ CUIIVK ~ ICIUMD G…
  • p. 589 …With a loss of 10°C superheat, and a limited flow (900 grams per hours), it…
  • p. 594 …flight a high loss of lifting gas caused the total ballast load ot 600 g~s…
  • p. 610 …g. Low brittle temperature h. High transparency to heat redie.tion Table I is a qualitative…
  • p. 625 …C"N-~.~- 8 "/)/A.,=_--.s:¥::J.i:;## PuRD.t.;f.T..t:Jte fiL relf! ----.... CA…
  • p. 630 …11A rt:~IA.t. - B.t.owN Pr.eex G£.A.5S "A1-e CHA/"'f1J4…
  • p. 646 …rate of rise in feet per minute G : g~oss lift in grams For our purposes…
  • p. 650 (Approximate) where G • gross load A chart, Figure 24, has beendrawn up, based on this equation…
  • p. 652 ~G = G X ~X (1 • K) K T where t::.. G = loss of lift G =gross…
  • p. 675 III II ! I rl G 01 NYU BALLOON PROJCT FLt8ht 5 DAT£ 6-5-4…
  • p. 680 …Fl G 36 NYU BALLOON PROJECT FLlGHT 7 D<ll-e: 7-2-47 E 0…
  • p. 683 …n..1m•tter Fl G.3 9 NYU BALLOON FROJtCT FLIGHT 8 D a. te 7…
  • p. 686 …to a thtmble a.nd attached to re1n forced pCltches at alterna.te .sea.m.s…
  • p. 688 …H.A.Smtth Inc. v.11th reinforced blowout pa.tches to vent 9Q.b when f1red…
  • p. 690 …G.M.. OO!"pol.yettHlent- balloon w1th 1ncend.1a. ry pa.tch on e~:~u a…
  • p. 713 …OBSTRUCTIONS TO AIR NAVIGATION A. WHITE SANDS, NEW MEXICO, PROV»>G GROUND -NEW YORK UNIVERSITY - RELEASE…
  • p. 731 …2. "Progress in Developing a Constant-Level Balloon", Report by Dewey and Almy Chemical Company, Cambridge…
  • p. 732 …Lugeon, Jean, "Le Poste Aerologique de la Station Centrale de Meteorologie a Payerne et les nourelles…
  • p. 742 …The automatic control is needed for flights lasting through a period in which day changes to…
  • p. 749 …1\\a Mr. o. c. Vinsea to C.B. Moore on rlait. 5/l'J/47…
  • p. 761 The follo'W1.n.g personnel lolere hired but later resigned: 1!.!.!! Robert 't:isnieff Robert…
  • p. 770 …diameter ballgons made from polyethylene .00411 polyethylene .008 11 saran • 00~25 11 aDd a fortisan…
  • p. 775 …g o! Ul ins":.tument coiilpany whicr. wo,.tld cor.struct the altitude control devices. A…
  • p. 779 …As a result of this preliminary study a sub-contn:.ct was given to H. A…
.u; a:s:e!T
II EXlSTE'iCE OF A SOU:m CHAN:fEl iN TRF AT"'C~PHERE
In ~eptember, 1944, 1 t occurred to me that there
is a s1~1lar sound channel 1n the atmosphere with the axis
at a height of about 45,000 teet, and that, with eource and
receiver plsced at th1e height, we might exceed the accepted
range.!! a a enormously UJ we had tn the ocean. ln other wot"da,
it might be -poat~ib~.e to detect sound halt way aro•.1nd the world.
~: ..
The fundamental data on this subject as revealed_dur1ng
a hur~ied search of the literature (mostly nrior to 19~0), ahow
that, for a t:voical large exoloe1on, there is at:dibility from
0 to 25 miles an1 froM 90 to 125 miles, with a zone of silence
from 25 to ~0 ~1lee. The accepted explanation of the total
collection of these dat:t is tbat tt1e 5T)eed of sound deore:ases
fro"'- about l 090 tt/see at the ~urtace to about 970 ft/sec at
about 45,000 feet, a:::d tt:cn inc:reases to abo:1t 1165 ft/sec
at a~ut 130,000 feet. (Reference 2)
Thu~ there 1~ a ~oun1 ~hannel in the atmosphere
with its axis at a ~ei;bt of aco~t 45,000 feot, nnd if both
sound source and 7-'aceiver are located at th!:: height, ".te
!!WY a.x:;>ect extr:aoro1nary !'lilnges and all the othor nseful
~heno~ena which have been found in the sound channel ln
the ocean. This means that the signals will have highly
eharaeter1st1c 1dent1fy1ng features anj that they will permit
aeou~te tr1an~ulat1on.
III ?ROBABLE 7lAXIJ:UM F\A~lGE
'l'he maxlmul'll N.nge ror sonic signalling 1n the
ataoapher1o aoum ehannel.w111 :1epend pr1Dt&r1ly on the
absorption coeff1c1ent, which 1a .the rate at wblcb the
acoustical energy 1a converted 1nto heat_by fr1ct1onal los~ea.
•ollow1ag Rayleigh (Rete~ence 3, P• 316), it MAy be calculated
that· the distance at Wb1ob·eound of.trequency 50 cycles ~er
aecoDd would be reduced 1n 1ntena1ty by the !aotor 7.5 by
the ettect or t'r1otion alone 1a about 24,000.m1lea at sea level,
aDd about '500 allea at 45,000 feet~ Aa these d1atancea
are ·1nverflely proportional to tbe square or the frequency,
they would be one hundred t1mes greater tor sounds of fJ"equeney
5 oyele., oer •econd, wbioh ha•e often 'been o'bee~ved when
large ex~loa1ona we~e •tud1ed.
•••••

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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.