Measurements of 55‐Mev omnidirectional trapped protons detected in a small region of the South Atlantic by nuclear emulsions flown on recoverable oriented Air Force satellites are reported for the period August 1961 to June 1964 between altitudes of 221 and 736 km. During the period August 1961 to June 1962, the data best fit a flux versus altitude curve J = 4.99 × 10−11 H4.792 protons/m2 sec Mev and is in good agreement with the variation of atmospheric density at these altitudes. H is the altitude over the South Atlantic measured in kilometers, and the time is the total time in orbit. No consistent slow increase of flux with time was observed as would be expected as the result of changes in atmospheric density. A sudden increase in flux was observed after the July 9, 1962, high‐altitude nuclear explosion Starfish, which is explained as consistent with a nonadiabatic redistribution of inner‐zone protons with an approximate 3.5° pitch angle change for L = 1.4 at the equator. The proton flux decays as expected on the basis of atmospheric ionization losses only, over a 2‐year period. The values of the trapped proton average atmospheric density
that fit the decay are 3×107, 7×106, 2×106, and 1×106 atomic electrons per cm3 for altitudes of 275, 350, 440, and 500 km.