XFLLOM4: (continued) eleuds which have bee the a which show, in fast, that as one goes from the relat! wistadle troposphere where we have the decrease of te with height, inte the stratosphere where we have therval regions, the suoke pafte which grow at ac puffs over Solloman Air Force Rase in the sumer ef 1949, This that when you got inte ths stable layer the diffnsion sloxar. Xow, what takes place still further en up is , matter of conjecture and, as I say, I would be inclinedite agree that the rate of mixing was sl:wer in this npper Olle But I really con't think that wa can say that definitely . WEILER: - co - oe 7 woe Oe yet. ase _— ~ ebtte tt “> ro "LLL these neasurexente.,,do thay actually dateraine a dinensional shape of the peff before and after? KELLOGG: There were three phototheodolites, and i$ was possible deterzine the shape, in effort wag rede to separate tha effect of stear. WELLER: Was there any indication of non-isotropical...I mean, any elongation of an axis in certain directions? KELLOG3s Yes, but toig almost a2lwsys in a borisontal e = Row és you know that ast of this was not due to isentropic. #0/