7
ae
#ue
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tape|
Ly
(1) the mezacou bpome cebzis waich does sot fall
tne first few nocws 22 acsigneu C77
out locally in
cue stvatouphere and
1% to tne tropusphere;
ic assumea to ve CIJ% for
Leua surface shotc ain 25% fo2 surface water shots anc 100%
for aivy ohots;
trovorpna ze;
“2) ali kiioton Vnot. ace agssi.yned to the
(4) it i: ascumed that the Latitudinal spread of
txoposphevic bomb cioucs is onsy Ld degrees with a sharp step
function ratner than a nocmal ervor curve divcribution and the
<ecidence time for tunis FaiLout is taixen to be one month as
described above.
Or. the basis of tnese assumptions, knowin, tne
yieids and types of vomb. Whicn nave veen fired, we estimate the
total stratospheric inveutory anc on the pasis of various
,easonable st-ratospneric sesidence cline py -edict the sfvatospheric
faliout over the earth's Tusface
vain Fa.L.
au averageu Latensity of
Figuce 9 Vives the stratospnecic inventory for
strontium-92 as Geauceda in this maine: up to January 1, 1959,
calculated on the vasis of two av vumecs cesider.ce times
5
and
It is interectinu, to note the tremendous vise in Octover of
last yeac due to the xussian test o
SL LRA'S
ix. the polar rezions.
‘bout a 69% increase due to ain ercimated 25 me,,atons, of fiesion
injected iato tne ctratosphere in tnat one month.
Tai. makes
"oO
oesible a searcning test of ali tne theories of stratospheric
te