Abstract
The vertical flux of primary protons and of alpha particles has been measured at Guam, Marianas Islands (λ=3°N) using a Čerenkov scintillation detector carried to a residual pressure of 6.1 g/cm2 by a Skyhook balloon. The primary alpha flux, J0α was found to be, J0α=18.0±2 particles/m2-sec-sterad at 0 g/cm2 atmos depth. The flux of primary protons, J0p was found to be, as an upper limit (without returning albedo correction), J0p=115±12 particles/m2-sec-sterad at 0 g/cm2 atmos depth, and as a lower limit (with returning albedo corrections), J0p=95±12 particles/m2-sec-sterad at 0 g/cm2 atmos depth. This flight completes an extensive latitude survey of the alpha and proton components by this laboratory using identical detectors at all latitudes. The alpha energy spectrum can be represented from 0.150 Bev/nucleon to 7.3 Bev/nucleon by {J0α(E)=(1.5)(415)E[1exp(80E3)](1+E)2.5,dE}{particles/m2secsterad,} where J0α(E) is the vertical flux of primary alphas with kinetic energy E (measured in Bev/nucleon). This energy spectrum is in excellent agreement with the measured low-energy alpha differential energy spectrum. Above 0.35 Bev/nucleon the alpha energy spectrum is accurately represented by J0α(E)=415(1+E)1.5 particles/m2-sec-sterad. The proton energy spectrum in the latitude range 0-41°N (15.2-4.0 Bev/nucleon) is well represented by J0p(E)=6600(1+E)1.5 particles/m2-sec-sterad. Thus the flux of protons and alphas has the same energy dependence over a wide range of energies. Values of the flux of splash albedo at λ=3°N are given and estimates are made of the magnitude of the returning albedo correction.