METEOROLOGICAL INFLUENCES ON Sr CONCENTRATIONS
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Fig, 2—IBy deposition, precipitation rate, and THI cross sections for
the storm of May 10,1963. Contours of reflectivity are given in units of
mm 5 m4,
curred about four to five months after the last recorded atmospheric
test.!’ in December 1962. The ®%Sr/Sr ratios for these four storms
were plotted together with the ratios obtained for the other storms
Sampled as part of this project in Pennsylvania, Oklahoma, Hawaii, and
California, These ratios are shown in Fig. 3 with the many total storm
ratios obtained by Kuroda™ in Arkansas rains. The apparent 50.5-day