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- W2045043336 abstract "The investigation of the long period fading of radio echoes from the moon has provided a new technique for the measurement of the total electron content of the ionosphere (Browneet al., 1956). This method is based on the measurement of the rotation of the plane of polarization of the radio waves produced by the magneto-ionic effect in the earth's ionosphere. Some preliminary results (Evans, 1956) indicated that the total electron content is approximately twice that which would be expected on the basis of a simple parabolic layer from pf́ data. In this paper a brief account of the technique is given together with a description of the method of analysing the records. The results of observations over a period of one year are then given. The technique is at present severely handicapped by the limited observing time imposed by the fixed (transit) aerial, and in consequence the results for some lunar months are poor. However where good results have been obtained, the ratio between the observed electron content and that in the parabolic model has always been in the region of 2: 1. There appears to be some evidence that the diurnal variation of the total ionospheric electron content is not completely regular, which is suggestive of tidal effects." @default.
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- W2045043336 date "1957-01-01" @default.
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- W2045043336 title "The electron content of the ionosphere" @default.
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- W2045043336 doi "https://doi.org/10.1016/0021-9169(57)90071-5" @default.
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