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- W2113110599 abstract "The seasonal changes in earth-current flow at Tucson, Arizona, have been determined from a study of the calm day diurnal-variation records for the three-year period 1932–34 obtained through the cooperation of the Department of Terrestrial Magnetism of the Carnegie Institution of Washington, the United States Coast and Geodetic Survey, the American Telephone and Telegraph Company, and the Mountain States Telephone and Telegraph Company. The records are of unusual interest because of the location of Tucson in the transition-belt where the diurnal variation of magnetic dip and intensity change from high-latitude to equatorial type. The diurnal variation in earth-current potential-gradient, as shown by a series of monthly hodographs also changes radically with season. During the winter the hodographs are nearly circular with the current-vector proceeding in two clockwise loops. During the summer they are elongated greatly along a line which corresponds closely to the magnetic meridian and the clockwise rotation of the vector tends to disappear at midday. A decided parallelism with the changes noted in the diurnal variation of the magnetic elements as recorded at the same station adds to the evidence linking the two phenomena together." @default.
- W2113110599 created "2016-06-24" @default.
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- W2113110599 date "1935-01-01" @default.
- W2113110599 modified "2023-09-26" @default.
- W2113110599 title "Seasonal variation in Earth-currents at Tucson, Arizona" @default.
- W2113110599 doi "https://doi.org/10.1029/te040i002p00183" @default.
- W2113110599 hasPublicationYear "1935" @default.
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