id WEXLER: high level storage. For example, it is possible for meteorologists to propose a reasonable mechanism. They can bring stuff down to Chile, in aball we say « veek, under proper cireusstances andgive you rain within @ wek. HOLZMAN: That is sefther an argusent for or egainst high level storage. I think that it would be interesting to notice that it gives a background information of the dfatribution. LIBBY: I think that we ought to make measurements anyhow though; they are easy to make. You bave « station in South Americas, dot you, Mr. Eisenbud? BISENEUD: Yes. WEXLER: Make the measurements and then go on from there and ewe if the meteorologists Can explain this particular rainfall, whether he has to involve high level érip or unusual transport across the equator. VOICE: Can't something be done to sake these fallout measurements sore useful in terns of rainfall and at the same time take very quantitative rainfall measticments to get some ides of how’ the radioactivity ie related to rainfall intensity--cr hae this been done? LIBSY: It bas been done. BILL: He hae charts plotted where they have barographes from fallout seasurenents and rainfall. That bas been done at Upshot-Knothole. What they didiivas alert three etations around the eountry to go out when precipitation starts and eollect rain at 20 uinute intervals for the duration of the precipitation. DUE ARCHIVES