-~16
«
Conclusion
Although, in principle, it is possible to plan a procedure
for predicting the removal rate of delayed fallout from the
stratosphere, in practice it is necessary to rely on the limited
observations available to make the most reasonable estinate.
It
is recognized, however, that because the actual dotails are being
‘omitted, the chance that serious errors are present becomes
greater.
It is felt that stratospheric sampling holds a key to a
more rational vitapegebset of the storage time.
The distribue
tion in tims vadtyS588,pes
restiy the meteorologist, with even his
maeegre inforzation, tepredict the desired quantities morereliably
than at present.
As a final word, it might be added that the neteorologist
stends to share in the knowledge which will be collected in the
solution of ths Strontiu--90 fallout problem.