Records of magnetic field as a function of altitude have been obtained from total‐field magnetometers mounted in two Aerobee sounding rockets which were fired from the seaplane tender USS Norton Sound in March 1949. The flights were made 60 miles apart at approximately 89° west longitude, 11° south latitude, or geomagnetic longitude 341°, geomagnetic latitude −1°. The first rocket, Aerobee Round A‐10, was fired on March 17 at 17h 20m 90th meridian time; Round A‐11 was fired on March 22 at 11h 20m 90th meridian time. In Aerobee A‐10 the field decreased between 20 and 105 km in accordance with the simple dipole field, while in Aerobee A‐11 a discontinuity of 4±0.5 milligauss was observed in the altitude range of 93 to 105 km.
These results (1) establish experimentally the existence of a current system in the E‐region of the ionosphere which is responsible for the diurnal variation of the earth's magnetic field at sea level; and (2) lend strong support to the dynamo theory of the daily magnetic variation which was originally proposed by Balfour Stewart and Schuster.