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Measurements are reported of the daily variations of meson intensity at Mawson, Antarctica ( lambda = 73 deg S), recorded by counter telescopes inclined at 45 deg to the vertical in each of north, east, south, and west directions. The results, together with those from a vertical teleseope, are examined and found to be inconsistent with an assumed common origin of the different directional variations in the interaction of am anisotropic primary radiation with the Earth' s dipole field.

Directional Measurements of the Daily Variation of Cosmic Ray Meson Intensity at l=73 °S.