Abstract

AbstractGuided by the working hypothesis that the Schwabe cycle of solar activity is synchronized by the 11.07‐year alignment cycle of the tidally dominant planets Venus, Earth, and Jupiter, we reconsider the phase diagrams of sediment accumulation rates in Lake Holzmaar and of methanesulfonate data in the Greenland ice core Greenland Ice Sheet Project 2 (GISP2), which are available for the period 10000–9000 cal. BP. As some half‐cycle phase jumps appearing in the output signals are, very likely, artifacts of applying a biologically substantiated transfer function, the underlying solar input signal with a dominant 11.04‐year periodicity can be considered to be mainly phase‐coherent over the 1,000‐year period in the early Holocene. For more recent times, we show that the reintroduction of a hypothesized “lost cycle” at the beginning of the Dalton minimum would lead to a real phase jump. Similarly, by analyzing various series of 14C and 10Be data and comparing them with Schove's historical cycle maxima, we support the existence of another “lost cycle” around 1565, also connected with a real phase jump. Viewed synoptically, our results lend greater plausibility to the starting hypothesis of a tidally synchronized solar cycle, which at times can undergo phase jumps, although the competing explanation in terms of a nonlinear solar dynamo with increased coherence cannot be completely ruled out.

Highlights

  • In hindsight, it is a mystery that the important paper of Vos et al (2004) has been so widely overlooked in the solar physics community

  • Guided by the working hypothesis that the Schwabe cycle of solar activity is synchronized by the 11.07-year alignment cycle of the tidally dominant planets Venus, Earth, and Jupiter, we reconsider the phase diagrams of sediment accumulation rates in Lake Holzmaar and of methanesulfonate data in the Greenland ice core Greenland Ice Sheet Project 2 (GISP2), which are available for the period 10000–9000 cal

  • We show that the reintroduction of a hypothesized “lost cycle” at the beginning of the Dalton minimum would lead to a real phase jump

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Summary

INTRODUCTION

It is a mystery that the important paper of Vos et al (2004) has been so widely overlooked in the solar physics community. In order to average (as far as this makes any sense with only two samples) over noise and geographic peculiarities of the two sites, in Figure 7e, we combine the remainders of Dye 3 and NGRIP, whereby the two individual contributions are weighted with the inverse of their standard deviation in order to give them approximately equal weights

Comparison of Schove’s data with radioisotope data
CONCLUSIONS
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