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).