cloud.
The H+6 wind profile was used and constent fall ratel
of .15,
' .57 and 2.1 m/sec, respectively,were used for the three parti€le sizes.
(Including the altitude dependence of fall rate is probably
¢n over-
specification, considering the uncertainty in the spatial varfatior.
of the wind). - Shown in Figure 3 is this envelope.
Taongi i§
definitely
affected by the Union fallout, but the other islands are outs|de the
fallout envelope.
.
+
DOE ARCHIVES
37