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[Paper Review] Solar dynamo as host power pacemaker of the Earth global climate

V. D. Rusov, E. P. Linnik|arXiv (Cornell University)|Jan 11, 2011
Solar and Space Plasma Dynamics21 references3 citations
TL;DR

The paper proposes that the solar dynamo, through a hypothesized axion-mediated mechanism, acts as a pacemaker for Earth's global climate by synchronizing solar magnetic variations with geophysical processes. It demonstrates that nonlinear oscillations in the solar tachocline magnetic flux correlate with Earth's magnetic field, rotation, ocean levels, and seismic activity, and that a bifurcation model of climate based on van der Pol–Duffing equations with a solar power pacemaker term accurately reproduces long-term climate trends, including glacial cycles.

ABSTRACT

It is known that the so-called problem of solar power pacemaker related to possible existence of some hidden but key mechanism of energy influence of the Sun on fundamental geophysical processes is one of the principal and puzzling problems of modern climatology. The "tracks" of this mechanism have been shown up in different problems of solar-terrestrial physics for a long time and, in particular, in climatology, where the solar-climate variability is stably observed. However, the mechanisms by which small changes in the Sun's energy (solar irradiance or insolation) output during the solar cycle can cause change in the weather and climate are still unknown. We analyze possible causes of the solar-climate variability concentrating one's attention on the physical substantiation of strong correlation between the temporal variations of magnetic flux of the solar tachocline zone and the Earth magnetic field (Y-component). We propose an effective mechanism of solar dynamo-geodynamo connection which plays the role of the solar power pacemaker of the Earth global climate.

Motivation & Objective

  • To resolve the unresolved problem of how small solar irradiance variations during the 11-year cycle drive significant climate variability.
  • To identify a physical mechanism linking solar magnetic activity in the tachocline zone to Earth's geophysical systems, including climate, rotation, and magnetic field.
  • To establish the solar dynamo-geodynamo connection as a fundamental pacemaker for Earth's global climate system.
  • To demonstrate that the solar power pacemaker mechanism is embedded in and essential for accurate long-term climate modeling.
  • To validate the model by showing consistent correlation between solar magnetic flux variations and Earth's climatic and geophysical parameters on multiple timescales.

Proposed method

  • Proposes that 57Fe solar axions mediate energy transfer between the solar dynamo and Earth's geodynamo via the inverse coherent Primakoff effect.
  • Uses a bifurcation model of Earth's climate based on the van der Pol–Duffing oscillator equation to describe nonlinear climate dynamics on annual and millennial timescales.
  • Introduces a climatic potential of the form $ U = -\frac{1}{2} \xi^2 \nu^2 + \frac{1}{4} \xi^4 \nu^4 $, with $ \nu \sim \Delta\omega/\omega $, to model rotational and thermal climate responses.
  • Applies the equation $ \xi m \dot{\nu} = -\mu [\xi^2 (\Delta t)^2 \nu^2 - \lambda] \xi \nu - \frac{1}{\xi \Delta t} \frac{\partial U}{\partial \nu} $ to describe the dynamics of Earth's rotational velocity and its link to solar forcing.
  • Introduces a time-lagged response (5 years) between Earth's rotational changes and global temperature, modeled via $ \nu \sim kT_{t - t_{\text{lag}}} $, to account for observed lags in climate response.
  • Replaces the time-derivative term in the model with a static equilibrium condition $ \partial_T U' = T^3 + a'T + b' = 0 $ for long-term (10,000-year) climate evolution, incorporating the solar pacemaker through renormalized parameters.

Experimental results

Research questions

  • RQ1What physical mechanism could explain the strong negative correlation between solar tachocline magnetic flux variations and Earth's magnetic field (Y-component) on decadal timescales?
  • RQ2How can small changes in solar irradiance during the 11-year cycle induce large-scale climate variability?
  • RQ3Can the solar dynamo serve as a pacemaker for Earth's global climate system through a coherent physical connection with the geodynamo?
  • RQ4What role does the axion-mediated energy transfer via the inverse Primakoff effect play in establishing solar-terrestrial climate coupling?
  • RQ5How does the inclusion of a solar power pacemaker term improve the accuracy of long-term climate models, particularly in reproducing glacial-interglacial cycles?

Key findings

  • A strong negative correlation exists between temporal variations in the solar tachocline magnetic flux and Earth's magnetic field Y-component, observed only at observatories where $ \delta Y/\delta t \propto \delta D/\delta t $, indicating a geodynamo-solar dynamo link.
  • The model shows that the solar power pacemaker mechanism, embedded in the bifurcation model, accounts for the observed 5-year lag between Earth's rotational velocity changes and global temperature shifts.
  • The bifurcation model of Earth's climate, when incorporating the solar pacemaker, reproduces the observed long-term trends in global temperature and ice volume with high accuracy.
  • The same nonlinear oscillator equation (van der Pol–Duffing type) describes both the solar toroidal magnetic field evolution and Earth's climate dynamics, indicating a unified physical mechanism.
  • The equilibrium form $ \partial_T U' = T^3 + a'T + b' = 0 $ on the 10,000-year scale confirms that the solar pacemaker mechanism is not masked but embedded in the model via parameter renormalization.
  • The model's ability to reproduce known paleoclimatic trends without ad hoc adjustments provides strong evidence for the physical reality of the solar dynamo-geodynamo connection as a climate pacemaker.

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This review was created by AI and reviewed by human editors.