论文标题
相干性和相位跳跃在施瓦贝周期中
Phase coherence and phase jumps in the Schwabe cycle
论文作者
论文摘要
在工作假设的指导下,即太阳能活动的雪瓦周期是通过潮汐主导的行星金星,地球和木星的11.07年对准周期的同步,我们重新考虑了Holzmaar湖中的沉积物堆积速率,以及甲烷硫酸盐盐(MSA)数据的100 000年000 cal-000 cal-000 cal-000 cals for giS2 cals for giS2 cal for Thate for giS2 cal for thate for giS2 cal。 bp。由于在输出信号中出现的某些半周期相跳跃很可能是应用生物学上证实的转移函数的伪像,因此在早期,早期的1000年期间,具有显性11.04年周期性的基础太阳输入信号可以被视为主要相位 - 相互关系。最近,我们表明,在道尔顿最低限度的开始时,重新引入了一个假设的“丢失循环”将导致真正的阶段跳跃。同样,通过分析$^{14} $ C和$^{10} $的各种系列是数据,并将它们与Schove的历史周期最大值进行比较,我们支持1565年左右的另一个“丢失循环”的存在,也与实际阶段跳跃相连。从概括方面看,我们的结果为潮汐同步太阳周期的起始假设提供了更大的合理性,有时它可能会跳动相位,尽管从非线性太阳能发电机和相干性增加的竞争解释不能完全排除。
Guided by the working hypothesis that the Schwabe cycle of solar activity is synchronized by the 11.07 years 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 (MSA) data in the Greenland ice core GISP2, which are available for the period 10000-9000 cal. BP. Since 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 years periodicity can be considered as mainly phase-coherent over the 1000 years period in the early Holocene. For more recent times, we show that the re-introduction 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 $^{14}$C and $^{10}$Be 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 non-linear solar dynamo with increased coherence cannot be completely ruled out.