Maybe it will be a residue sort of a thing that ve can
aktribute
to nothing elsey but diffusion, but somehow Ifeel that
tatively it will not improve cur knovledge of turbulent
Tn view of the fact that I still maintain that in a
atao-
sphere it's probably very much lover than the otber p
that are spoken about with isentropic notions, and in
unstable
atmosphere much lover than penetrative convective
such as thunderstorns.
.
You would say then, in view of the sort of thing that
tud's doing and Machta {s doing = and alec collect more
Yes, and I go along with Will's reccamendation except I
think I'd dignify 1t teythe word experiment; Just say,
in the formof herleontal traverse by aireraft =- make
t
travaersss by any means whatsoever - stroraftox belloon fas
they become available,
This ts for elouis - oot nacensnriy fer streteapherey ft foe
ssccccoesethis 1s not necessarily forradicective clouds in the
etretoaphare, but for the lover ones vintch «
WEXLERs
No, This is the whole probles. That's the fallout we’
discussing.
KRAMISH:
Given a radicactive cloud placed in the stratosphere,
it |
ever achieve a uniform distribution, and if so, how
parericast of Eneray
bes
mate
“ttina
vom
1 he
ygiesa
a/4