Abstract
A BIENNIAL oscillation in tropical stratospheric winds1–3 and total amounts of ozone4–6 has been well documented during the past few years and its discovery has led to a re-examination of much of the earlier work on biennial oscillations in surface temperature, rainfall, tree rings, lake levels and other parameters which depend on conditions in the troposphere7. I have argued elsewhere8 that the oscillation in the stratosphere is caused by changes in the troposphere, and this argument is in line with much of the present thinking about tropospheric–stratospheric interactions, which holds that the lower stratosphere receives its driving energy from below9–11. If this reasoning is correct then there must be sought a source for the 26-month oscillation in the tropospheric heat engine. One possibility is some type of internal oscillation; another is that the incoming radiation which drives the tropospheric heat engine (approximately 3000 Å to 2µ is modulated with a 26-month oscillation.
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NEWELL, R. 26-Month Oscillation in Atmospheric Properties and the Apparent Solar Diameter. Nature 204, 278–279 (1964). https://doi.org/10.1038/204278a0
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DOI: https://doi.org/10.1038/204278a0
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