Abstract
II. THE title of Paper IV.—“Storms in Bengal, accompanied by increased Atmospheric Pressure and the Apparent Reversal of the Normal Diurnal Oscillation of the Barometer,” by Prof. J. Eliot,—must necessarily appear somewhat strange to those accustomed in our latitudes to the frequent masking, if not actual reversal, of the normal diurnal oscillation, by the large and rapid non-periodic oscillations to which the atmospheric pressure is subject.
Article PDF
Rights and permissions
About this article
Cite this article
Indian Meteorology 1 . Nature 28, 428–430 (1883). https://doi.org/10.1038/028428a0
Issue Date:
DOI: https://doi.org/10.1038/028428a0