UNCLASSIFIED
at the Eniwetok Proving Ground. With known meteorological data such
a technique will successfully quantify the area of faliout and indicate
qualitatively the relative intensity cf radiation.
Precise determination of the fallout area requires consideration
of many complexmeteorological parameters. However,from the above
analysis a practical field teol cas be developed that in most cases will
satisfactorily define the area of interest.
REFERENCES
1.
Approved by;
E.R, Lphine
E.R. TOMPKINS
Zz.
3.
Head, Chemical Technology Division
For the Scientific Director
Dallavalie, I.M.
New Yo.k, N.Y.,
Srunt, D.
Physical snd Dynamical Meteorology, Cambridge
University Press, London, T94T.
A Siudy of the Atmosphere Between 30,000 and 160,060 Feet
Tereliminary reports, mel of Naval Operatieas, AerologyService
Section, Washington D.C., September 1948,
4.
Smithsonian Physical Tables, 1954.
5.
Schuert, E.A.
<A Fa:lout Plotting Device, U.S. Nawal Radiological
Defense Labcratory Technical Report USNRDL-~127, February 1957.
~14-.
palestadietes
Micromeritics, Pittman Publishing Corporation,
-
~15-
rte Rene
ae eeer