Abstract
Prof. E. V. Applet on and K. Weekes have shown the existence of a lunar tide in the Kennelly-Heaviside layer, which is accompanied by a relative pressure oscillation 6,900 times as large as the corresponding lunar pressure oscillation at ground-level.
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Points from Foregoing Letters. Nature 142, 78 (1938). https://doi.org/10.1038/142078a0
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DOI: https://doi.org/10.1038/142078a0