Abstract
Meteorological conditions prevailing over and west of Bombay on the four days on which Bhatet al. (1974) made measurements of radon concentration at different altitudes from the surface to 3·7 km and distances of 0–50 and 350–400 km west of Bombay, do not appear to support their conclusions about airmasses.
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More From: Proceedings of the Indian Academy of Sciences - Section A
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