212

PERKINS, THOMAS, AND NIELSEN

centrations of "y and !“Sb during January 1964 help explain the ob-

served high fallout rates of these radionuclides during the summer of

1964 (see -Fig. 7). The relatively low concentrations of '“*Cs in the
stratosphere are in accord with the '“Cs to '3’Cs ratio measurements

on biological samples,’ which show a large drop in this ratio since

1961 and indicate that a major injection of “Cs into the atmosphere

occurred prior to the past test series.
Stratospheric samples were available which covered latitudes

from about 26 to 70°N at longitudes of 97 to 146°W. This covers an
area from southern Mexico to northern Alaska. These samples were

collected between Jan, 8, 1964, and Feb. 18, 1964. In Fig. 10 the ratios
10

—

=

57 ,_95Nb

T

Le

a ™

=

—

]

[

|

Ll

J

Bay

Po

Le

_

[

E —

3

—

z

_

Lo

<

1.0 — ——

r

0.1

0.5 &

_

4

_L

{

3

l

mSb

—

—

Hc,

—-_

—

=

0. C-—lL_|_

||

a

T

>

Wha

a

0.5 —

|

yin

=

_1
I24ch

=

=

7

Loft

= PC]

-

0.05
10 =

o_o oF

Pe

—

—

=

a

2nig

20

|

We,

- —

4

0.01 c

0.001

4

|

a

—
~

|

—

=

Lo

= =

Jj

© 0.001

Mee

5

o

a

_

1

=—

2 0.01 &=
2

i

a

—

{

_

=~

5

=
|

=

4

_

=

0.01

—_—

=

>

—
“

ro

1

—

on

—

T-

4
4

Ole

we

10

|
L
{
I
30 40 50 60
DEGREES NORTH

ke

|

1
70

20

30 Oo 50 50
DEGREES NORTH

70

Fig. 10—Ratios of the concentrations of various airborne radionu-

clides to 9’7Cs as a function of latitude (stratospheric samples).

Select target paragraph3