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Chapter 4

METHODS AND ANALYSIS
The photographic study of cloud-rise phenomenadiffers in several important respects
from the customary aerial survey or photogrammetric mapping problem. It is not enough
simply to establish accurate scale factors for distance.

Customary mapping procedures

always reduce the three spatial dimensions to two by employing a system of contours to
represent the relatively slight variations in the third. Here refuge cannot be taken in
such a device; the three spatial dimensions, and also time, must be considered as four

separate, independent, and irreducible variables. A complete analysis of all phases of
this problem would be laborious and unjustifiably expensive; even a limited study, however, requires accurate and complete controlof all four variables for every photograph
exposed. In addition, it requires experience and judgment.on the part of the analyst to:
(1) interpret the séries of pictures, (2) identify irregularities in the poorly defined and
sometimes nebulous cloud surface, (3) evaluate the relative importances of prominences
in the cloud, and (4) estimate probable features which-are hidden from the camera.

4.1 SPATIAL CONTROL |

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It is necessary to know thefollowing for each photograph: (1) horizontal distance .
from ground. zero, (2) altitude of the camera platform, (3) horizontal aiming angle
‘(bearing), (4) vertical aiming angle (tilt), (5) focal length of the lens, (6) distortion
‘ characteristics of the camera,. (7) location of the optic-axis on the film (fiducial marks),
and (8) earth curvature and atmospheric refraction.
In addition to the above, it is desired to make sure that the field.of view of the
camera is large enough. A photograph in which cloud-cover, perspective difficulties
and curvature-refraction effects are all minimized is preferred. These are contra-

PINE SP PRL

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dictory effects, and the optimum distance for multimegaton bombs is of the order 75
to 150 miles.

In practice, Items 2, 4, 5, 7, and 8 are usually quite well known. Hem 6 is

neglected; Item 1 is known to about +2 percent; but Item 3 is too poorly known

(+ 4 degrees or so) to permit any true three~dimensional analysis. Lack of this information requires that the cloud phenomenabeevaluated in the vertical plane through
ground zero. The loss of any of these data, for any given photograph, seriously impairs:
the value of that picture to the study.
Data regarding camera position for the Castle detonations were derived from the
navigation logs furnished from the field.. The given data were plotted for each mission
"as a series of arrows originating at the given position and terminating at the expected
position 1 minute later. Since the terminus almost invariably differs from the actual
position given by the log for that time, by 1 to 10 miles, it must ‘be concluded that the
data are not internally consistent.

Therefore, a smoothed curve is drawn through the

data to represent the probable course of the ship. An adjusted time scale is constructed
along this curve, with equal increments of distance to take account of the nearly constant
velocity and with minimum deviation from the logged time scale. This curve is felt good
17

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