APPENDIX "Dp"
PROGRAM 4.0 ~ CLOUD PHYSICS AND METEOROLOGY
1.

GLOUD PHYSICS
a,

‘This portion of the program was undertaken in order to fully document

atomic clouds during their rise in order to obtain information of use in operational
air drops, and to allow studies of entrainment of air, turbulence, and diffusion to
‘be made.

In addition, it was desired to determine in some detail the temperature

and water vapor content of atomic clouds in order to evaluate the possibility of
producing artificially stimulated precipitation,

2b.

Photographic documentation of the rising atomic clouds was carried on

both from the ground and the air for DOG, EASY and GEORGR shots.

On DOG shot, the —

ground cameras failed to obtain a record due to a low overcast, but adequate cover-

age was obtained from the air.

Satisfactory ground and air coverage was obtained

on both EASY and GEORGE shots and these films are now being processed,

Rough analy-

sis of data taken by ground observers, using theodolites, on GEORGE shot showed that
the third shot attained an altitude of 26,200 feet in 1 minute and 45 seconds, an

altitude of 47,500 feet in 3 minutes and 33 seconds, and a final altitude of 70 ,000
feet in 1l minutes and 4 seconds,

The radius of the cloud at26,200 feet was 1.2

miles, at 56,500 feet was 3,2 miles, and at 70,000 feet was 5.0 miles.

Tb is inter.

esting to note that the bomb cloud requires from 11 minutes to 12 minutes to reach
maximum altitude regardless of yield.

It is also interesting to note that GEORGE

shot was the first cloud to actually penetrate the tropopause,
c.

In order to study the temperature and water vapor content of the atomic

cloud, the K@llsman Instrument Company developed a new acrograph which was capable of

operation in drone aircraft on a fully aulomatic basis.

A total, of thirty aerograph

flights were made in and around atomic clouds arising from the three shots.
d.

Preliminary analysis of a portion of the flights reveals no striking

temperature or humidity features in the atomic cloud as compared to ordinary clouds,

The temperatures as indicated by the aerograph were lower inside the cloud than in
the environment.

This apparent

whether it is real.

anomaly is being investigated further to determine

Study of the indicated air speed at the time of entrance into

the cloud revealed that in the majority of the traverses a sudden increase in the
air speed was experienced although the power, controls, surfaces, etc. remained at
constant settings,

@. :The humidity traces revealed rather low humidities in the atomic cloud,

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