= =e woLER9 s eee Well, as I see this probles, Will, you measure a distribution of stuff at the ground and you'd like to it got there. You know there it starteds you knoy the distrita- tion is the United States, and you'd like te fill in the/intervening mechanism that brought 14 dow. And you say this/{fs an air burst, so we don't have to worry about fallout. Wha} then are the mechaniens that you can invoke? You would like invoke turbulent diffusion of which aduittedly ve mow little. There is some disagrement as to the intensity bably, differing by orders of magnitute. KELLOGG: I'd like to say that we'd perticularly like to know this the stratosphere which we could obtain from tracking the clouds in the Marshall Islands. . Toms Could I get clarification en that? I don't quite see particularly wish to knov this in the stratosphere for ¢ reason — it doesn't seen to be terribly consequential to local fallout problen and, for the wrld vide fallout, some to Re one can say, well, this dust 1sgoing to be distributed extremely broadly and there's good evidence 1% canes dow very alowly. I can see vhere ’ this might be interesting, tut I don't quite understand it fits into the Sr problem. KELLOGG: Um base, | Well, as I said earlier, I'm not ever ashemed o giving a meteorological reason for wanting to find scusthing * ooh oF ™ al / . : Mote H/G