Fis
Wee pe
we
“ARRETR:
motions rather than turbulent diffusion?
KELLOGOs
The herizontal elonczation was sesuned ta be due to shear, and
(contimed!
wo it was only the spread at right angles to the shear that was
considered,
When I drew this, I was isplying that we've
eliminated the effects of shear from the data.
VOICE:
The Signal Cerpe has been trying to measure width by setiing
up smoke trails from reckets, and hes been unsueceseful because
the diffusion rate is so great that they den't even have a chance
to photegraph it.
Thia is the heriszontal?
Yow this ig just disatpation of the vaper trail itself, with the
*"OXICKs
smoke trail,
KELLOGG:
I've heard this too.
RB, PLESSET:
It just breaks spart.
VOICE:
De you think this in the region below 100,000 feet; or is this
up in the very high region above the ozone layer?
VOICEs
TI don't think it went up that high.
KELLOOGs
Then they'd be getting inte a region of steep lapse rate again.
‘Thirty-five siles.
Tive had to cespress it because of the sise of the blackboard.
This is the 35 afles here, end then we get « decrease of tenpera~
ture with height, and we have very good evidence for a lot of
Ry
DOE ARCHIVES