On February 28, 1963, over in Arizona,
U.S.A., a constellation of seven angels appeared to a man named William
Marrion Branham in the form of a ring shaped-Cloud. These seven angels
came from the presence of God revealing to him the hidden mysteries that
were sealed in the Book of Daniel and the Book of Revelation. This was
to inform the people of God of the perfect will of the Father in
preparation for the oncoming millenial reign of Jesus Christ upon this
earth. It was as they left Brother Branham that they formed this
mysterious cloud which Life Magazine had featured in their May 17, 1963
issue and Science Magazine in their April 19, 1963 issue. The original
glossy prints reveal the full face of the Lord Jesus Christ as the
picture is viewed from the right side angle “like unto the Son of Man,
His head and His hairs were white like wool, as white as snow”
(Rev.1:13).
Life Magazine
Life magazine
May 17 1963
p.112
...And a High Cloud Ring of Mystery
Hovering like a giant's smoke ring, a
great cloud appeared at sunset over Flagstaff, Ariz, last Feb. 28 and
set off a continuing scientific mystery. Watchers struck by the cloud's
odd shape and huge size, took pictures, like these four, at different
times and from widely scattered locations in the state.
... more ...
Dr. James McDonald, a meteorologist at
the Institute of Atmospheric Physics in Tucson, has been accumulating
the pictures. Using them as the basis for trigonometric calculation, he
has made a startling discovery that the cloud was at least 26 miles high
and 30 miles across - "a lot higher and bigger," he says, "than a cloud
should be." The circle was too high to be made by a jet plane, and so
far as Dr. McDonald can determine, there were no rockets, rocket planes
or bombs being tested nearby that day. He hopes anyone else with
pictures will lend them to him, for he would like some more clues about
the cloud 26 miles up - no water droplets exist at that height to make a
cloud.
The photographs on the following pages were scanned from p.112 of Life magazine May 17, 1963.
Science Magazine
Science Magazine
19 April 1963 Vol. 140 No. 3564
Cover Story:
Ring-shaped cloud seen at sunset on 28
February 1963 in northern Arizona and areas of nearby states. The
height, as estimated from four photographs made in Tucson, Arizona,
about 190 miles to the south of the cloud (which appeared overhead near
Flagstaff), is about 35 kilometers. This photo was taken by Clarence E.
Peterson of Bremerton, Washington, while he was looking almost due north
from near Camp Verde, Arizona.
The unusual nature of the cloud was
evident to observers who noted its striking luminosity long after the
sun had set at ground level. It was at least 11 kilometers higher than
the upper limit of possible jet contrail formation, and was at least 5
kilometers higher than previously reported nacreous clouds of the arctic
type. Its true nature is still unknown; more photos are being sought
for triangulation purposes. See page 292.
Stratospheric Cloud over Northern Arizona
Abstract. An unusual ring-shaped cloud
was widely observed over northern Arizona near sunset on 28 February
1963. From a large number of observers' reports it is known to have
appeared overhead near Flagstaff, Arizona. From initial computations
based on four photos taken in Tucson, 190 miles south of the cloud, its
altitude was approximately 35 kilometers. The most distant observation
reported was made 280 miles from the cloud. The cloud remained sunlit
for 28 minutes after local sunset. Iridescence was noted by many
observers. Tentatively, the cloud may be regarded as similar to a
nacreous cloud; but its unusually great height and unusually low
altitude, plus its remarkable shape, suggest that it was a cloud of
previously unrecorded type.
Near sunset, on 28 February 1963, a
cloud of unusual configuration and coloration was observed in widely
scattered localities in Arizona and some surrounding states. The cloud
took the form of a large oval ring (clear in the middle) with the long
axis running north and south (Fig. 1 and cover photograph, this issue).
It remained brightly illuminated well after the sun had set on high
cirrus clouds to the west. From Tucson, 190 miles to the south, its
angular elevation appeared to be about 6 degrees. A rough computation of
its height, based on sunset geometry, (1) made immediately after the
cloud entered the earth's shadow, led me to appeal by press and radio
for confirmatory reports in order to establish the approximate location
and to secure descriptions from the largest possible number of other
observers.
From approximately 150 reports, many
communicated by persons well aware that they had seen a type of cloud
unprecedented in years of skywatching, it was quickly established that
the cloud lay overhead in the vicinity of Flagstaff, Arizona, that it
exhibited iridescence of the sort associated with stratospheric nacreous
clouds in the arctic (2,3), and that its internal structure was very
peculiar.
To observers nearly underneath, the
colors green and blue were visible, and a pinkish cast was noted at
times. A fibrous texture, described by several independent observers as
resembling a "wood grain" appearance, was present over much of its
northern extent, but its southern end was denser and more cumuliform.
Its overall shape was compared by some (ranchers) to a horseshoe or a
horsecollar if it was viewed from south; from the north it appeared as a
closed loop with a long thin trail that could be seen extending
northward, from the oval, and several observers in that sector compared
its shape with that of a "hangman's noose." The cloud was seen from
distances as great as 280 miles (near Douglas, Arizona and Albuquerque,
New Mexico, respectively).
Many observers reported a second cloud
off to the northwest of the main cloud, with shape very much like that
of the main cloud, but only about a quarter as large. Correctness of
these reports has been established from some of the first photographs
that have come in from northern Arizona. The cloud was evidently moving
generally south-eastward, though visual reports are in some conflict on
this point; this point can only be resolved from further studies by
triangulation. By fortunate coincidence, the cloud appeared within a few
tens of miles of the U.S. Weather Bureau radiosonde station at Winslow,
Arizona, and a high-altitude sounding had been completed there only an
hour before the appearance of the cloud. A jet stream lay almost
directly under the cloud and over Flagstaff, and there were peak winds
of 98 knots from the northwest occurring over Winslow at an altitude of
about 11 kilometers.
The radiosonde run terminated at the
13-millibar level of atmospheric pressure (about 29 km), where the
temperature was -46 degrees C. There was very little direction shear in
the Winslow wind sounding, a condition known to favor formation of
mountain waves and believed to be conducive to nacreous clouds, at least
in Scandinavia (2). It is possible, therefore, that the San Francisco
Peaks just north of Flagstaff disturbed the flow so that wave motion was
set up in the stratosphere, but this remains a conjecture, pending
further study of reports of first appearance. Whereas some recent
studies (4) suggest strong local stratospheric cooling as a prerequisite
for the formation of nacreous clouds, the sounding at Winslow showed
little departure from average temperature conditions in the lower and
middle stratosphere.
Photogrammetric analysis of the four
photographs known to have been taken in the Tucson area have yielded
elevation angles of the near point ranging from 5.9 to 6.2 degrees.
Because the exact range to the nearest point of the cloud is not yet
known to better than 10 or 15 miles in 190 miles, the exact height
cannot yet be determined. However, the cited elevation angles plus
allowance for earth curvature give a cloud height of 35 kilometers,
possibly a bit higher if the range to the near point proves to be
greater than 190 miles. This height is distinctly greater than that of
reported Scandinavian nacreous clouds. Photogrammetric heights obtained
over many years by Stormer and others (2,3) are no higher than 30
kilometers, and the majority lie between 22 and 28 kilometers. The
estimated height of 35 kilometers rules out the possibility that the
Flagstaff cloud could have been the condensation trail from a jet plane.
The present American altitude record, made under the most favorable
conditions directly above the home field by a Lockheed F-104 in 1959, is
103,395 feet (31.6 kilometers). Perhaps more conclusive is the fact
that the upper limit of height for possible contrail formation (5) as
indicated by the sounding from Winslow was just under 24 kilometers at
the time of the cloud's appearance.
These preliminary indications mark the
Flagstaff cloud of 28 February as a most unusual phenomenon of
considerable meteorological interest. Requests for photographs, still
being made at time of this writing, have already brought promises of
photographs from a total of 16 sites reasonably well dispersed around
Arizona, so fairly precise data on the cloud's height, shape, and
dimensions should be obtainable by triangulation. A conflict between
heights estimated from the Tucson photos and from sunset geometry is
under study (the indicated height based on available reports of fadeout
time is about 25 kilometers). Premature fadeout may have been due to
cirrus clouds between the cloud and the ray- tangency point, computed to
lie at or very near Los Angeles.
The hydrodynamics of the field of
vertical motion that produced such a toroidal cloud form are very
puzzling. Present estimates give the closed oval a length of about 60
kilometers and a width of about 30 kilometers, with a ring cross section
of perhaps 3 to 4 kilometers in the horizontal. I am not aware that a
cloud of such form and size has been observed at any level within the
atmosphere before. Interesting questions about the source of the
requisite water vapor are posed by its unprecedented altitude. (6)
James E. McDonald Institute of Atmospheric Physics, University of Arizona, Tucson
1. S.K. Mitra, The Upper Atmosphere (Asiatic Society, Calcutta, ed.2, 1952).
2. E. Hesstvedt, Geofys. Publikasjoner Norske Videnskaps. Akad. Oslo 20, No. 10 (1959).
3. A. Y. Driving, Bull. Acad. Sci. U.S.S.R. Geophys. Ser. 3, English Transl. (1959), pp. 279-286.
4.
Y. Gotaas, Geofys. Publikasjoner Norske Videnskaps Akas. Oslo 22, No. 4
(1961); A. Y.Driving and A. I. Smirnova, Bull. Acad. Sci. U.S.S.R.
5. H. Appleman, Bull. Am. Meteorol. Soc. 34, 14 (1953).
6.
I thank Leon Salanave for alerting me to the cloud when it became
visible in the Tucson sky and for further technical assistance, and I.
E. Daniels and C. E. Peterson for permission to reproduce their
photographs. The cooperation of the numerous Arizonians submitting
reports is gratefully acknowledged.
Supported by the Office of Naval Research under contract NR 082-164.
20 March 1963
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