Abstract
High-resolution spectra of Jupiter's decametric S-storms are studied with an acousto-optical radio spectrograph operating over the frequency range 20–30 MHz. In 1985–1989 20 S-storms were recorded in the Io-B region. There is only a slight average zoning effect of certain types of fine structure in the Io-B region, with sporadic S-bursts occurring most often in the early CML values, and S-trains in the late values. Emissions of type N and its variants occur at lower values of the Io phase than S-emissions and their variants. There is no exact storm-to-storm correspondence, nor any Io-B-centered zones in which the various types of fine structure could be accurately placed. Every storm is different and has a ‘signature’ of its own. An important exception is formed by the wide-range quasi-periodic FDS-S storms that occur at the edge of the Io-B region with Io phase values greater than 80 ‡. These are outstanding storms in which the individual bursts may extend across the full spectral width of 20–30 MHz and be repeated in rapid succession at quasi-periodic rates of 20–40 s−1. It is suggested that these be referred to as type Q storms. It is estimated that only 10% of the S-burst types are recorded so far.
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Riihimaa, J.J. Evolution of the spectral fine structure of Jupiter's decametric S-storms. Earth Moon Planet 53, 157–182 (1991). https://doi.org/10.1007/BF00057430
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DOI: https://doi.org/10.1007/BF00057430