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Spectral characteristic of mid-term quasi-periodicities in sunspot data

Frick, P.; Sokoloff, D.; Stepanov, R.; Pipin, V.; Usoskin, I. (2019-12-25)

 
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URL:
https://doi.org/10.1093/mnras/stz3238

Frick, P.
Sokoloff, D.
Stepanov, R.
Pipin, V.
Usoskin, I.
Oxford University Press
25.12.2019

P Frick, D Sokoloff, R Stepanov, V Pipin, I Usoskin, Spectral characteristic of mid-term quasi-periodicities in sunspot data, Monthly Notices of the Royal Astronomical Society, Volume 491, Issue 4, February 2020, Pages 5572–5578, https://doi.org/10.1093/mnras/stz3238

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This article has been accepted for publication in Monthly Notices of the Royal Astronomical Society ©: 2019 The Author(s) Published by Oxford University Press on behalf of the Royal Astronomical Society. All rights reserved.
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doi:https://doi.org/10.1093/mnras/stz3238
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https://urn.fi/URN:NBN:fi-fe202001172528
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Abstract

Numerous analyses suggest the existence of various quasi-periodicities in solar activity. The power spectrum of solar activity recorded in sunspot data is dominated by the ∼11-yr quasi-periodicity, known as the Schwabe cycle. In the mid-term range (1 month–11 yr) a pronounced variability known as a quasi-biennial oscillation is widely discussed. In the shorter time-scale a pronounced peak, corresponding to the synodic solar rotation period (∼27 d), is observed. Here we revisit the mid-term solar variability in terms of statistical dynamics of fully turbulent systems, where solid arguments are required to accept an isolated dominant frequency in a continuous (smooth) spectrum. For this, we first undertook an unbiased analysis of the standard solar data, sunspot numbers and the F10.7 solar radio flux index, by applying a wavelet tool, which allows one to perform a frequency–time analysis of the signal. Considering the spectral dynamics of solar activity cycle by cycle, we showed that no single periodicity can be separated, in a statistically significant manner, in the specified range of periods. We examine whether a model of the solar dynamo can reproduce the mid-term oscillation pattern observed in solar data. We found that a realistically observed spectrum can be explained if small spatial (but not temporal) scales are effectively smoothed. This result is important because solar activity is a global feature, although monitored via small-scale tracers like sunspots.

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