Schwabe, Gleissberg, Suess-de Vries: Towards a consistent model of planetary synchronization of solar cycles
arXiv:1910.10383 · doi:10.22364/mhd.56.2-3.18
Abstract
Aiming at a consistent planetary synchronization model of both short-term and long-term solar cycles, we start with an analysis of Schove's historical data of cycle maxima. Their deviations (residuals) from the average cycle duration of 11.07 years show a high degree of regularity, comprising a dominant 200-year period (Suess-de Vries cycle), and a few periods around 100 years (Gleissberg cycle). Encouraged by their robustness, we support previous forecasts of an upcoming grand minimum in the 21st century. To explain the long-term cycles, we enhance our tidally synchronized solar dynamo model by a modulation of the field storage capacity of the tachocline with the orbital angular momentum of the Sun, which is dominated by the 19.86-year periodicity of the Jupiter-Saturn synodes. This modulation of the 22.14 years Hale cycle leads to a 193-year beat period of dynamo activity which is indeed close to the Suess-de Vries cycle. For stronger dynamo modulation, the model produces additional peaks at typical Gleissberg frequencies, which seem to be explainable by the non-linearities of the basic beat process, leading to a bi-modality of the Schwabe cycle. However, a complementary role of beat periods between the Schwabe cycle and the Jupiter-Uranus/Neptune synodic cycles cannot be completely excluded.
arXiv comment11 pages, 4 figures, final version as published
References in corpus (3)
Cited by in corpus (6)
- How much has the Sun influenced Northern Hemisphere temperature trends? An ongoing debate
- Shaken and stirred: When Bond meets Suess-de Vries and Gnevyshev-Ohl
- The planetary theory of solar activity variability: a review
- A synchronized two-dimensional model of the solar dynamo
- No evidence for absence of solar dynamo synchronization
- Synchronizing the helicity of Rayleigh-Bénard convection by a tide-like electromagnetic forcing