Abstract
Abstract. The Australian Bureau of Meteorology (http://www.bom.gov.au/climate/mjo, last access: 9 February 2023) states that “The Madden–Julian Oscillation (MJO) is a major fluctuation in
tropical weather on weekly to monthly timescale. The MJO can be
characterized as an eastward moving `pulse' of cloud and rainfall near the
Equator that typically recurs every 30 to 60 days.” Early descriptions of
the MJO were contained in two papers by Madden and Julian (1971, 1972). This paper relates the story of developments in tropical meteorology in the 1960s that led to those two papers. The decade saw the first unambiguous
identification of large-scale, theoretically predicted, tropical waves. Spectral analysis was used effectively by researchers to link observations
with the theoretically expected features of these waves. At the same time,
longer time series of observations, faster computers, and an algorithm
designed to speed up Fourier transforms, vital for spectral analysis, all
became available. These developments set the stage for the oscillation to be recognized.
Subject
History and Philosophy of Science,General Earth and Planetary Sciences
Reference52 articles.
1. American Meteorological Society (AMS) and World Meteorological Organization (WMO): Proceedings of the Symposium on Tropical Meteorology, University of Hawaii, Honolulu, USA, 2–11 June 1970.
2. Atkinson, G. : Discussion following R. A, Madden’s paper, Wave Disturbances over the equatorial Pacific during the Line Islands Experiment, in: Proceedings of the Symposium on Tropical Meteorology, University of Hawaii, Honolulu, 2–11 June 1970, AMS/WMO, 1970.
3. Cooley, J. W.: The re-discovery of the fast Fourier transform algorithm,
Microchim. Acta, 3, 33–45, 1987.
4. Cooley, J. W. and Tukey, J. W.: An algorithm for the machine calculations
of complex Fourier series, Math. Comput., 19, 297–301, 1965.
5. Deland, R. J.: Some observations of the behavior of spherical harmonic
waves, Mon. Weather Rev., 93, 307–312, 1965.