Abstract
In this paper the data for the potential‐gradient at Poona collected on undisturbed days during September 1930 to December 1938 have been considered. The basis of these data is the continuous record of the Earth's electric field which was obtained here photographically. The undisturbed days at Poona are few and far between. A brief note on topography of the place and the general atmospheric conditions prevailing here is given below:
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