surrounding the point of detonation, and no cloud, colum, or surge is
formed.

D.

Effect of Meteorological Conditions on the Cloud.
Four different types of action upon the atomic cloud can re-

sult from the winds.

When the wind structure is sufficiently large to

embrace the whole cloud, gross movement occurs, i.e., the cloud as a
whole moves in the direction in which the wind is blowing.

When it is

just, or very nearly, as large as the cloud, it helps to move it, but

tends also to distort it as a whole.

When the winds are appreciably

smaller scale than the cloud, they cause the cloud to diffuse and lose
its shape, because of eddy currents and dilution with clean air.

Shear,

the fourth action, tends to string out the cloud in ribbons by vertical
deformation.

The effect of wind shear upon a single radioactive par-

ticle that is falling from its position at the time of stabilization is
one of lateral translation.

The amount of this lateral translation

relative to the main axis of travel is a fimction, within any cloud
segment of the wind speed of the segment and the length of time a particle spends falling through that segment.

Some of these air movements

tend to prolong the time that the large particles are in the air, increasing the horizontal translation by vertical wind motion during the
free fall response to gravity.

Particles that range in size from 100 to 5,000 microns are most

likely to fall out within local fall-out contours from large yield
detonations, although some smaller particles are also found.

The par-

ticle densities lie within a very narrow range of 2.5 to 2.8 gn/ec for
Nevada tests, while at the Pacific Proving Ground they average 2.4 and

range from 2.8 to 1.8 gm/ec.

When the densities are essentially the

same, the free fall rate is a function of particle size and atmospheric
density.

If constant particle density is assumed, the variation in the

rate of fall from different cloud heights can be determined from Figure
5.

Evidence indicates that from 50% to 90% of all radioactive particles

in a fall-out area are within the size range of 50 to 1,000 microns in

22

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