Reconstruction of Solar Extreme Ultraviolet Flux 1740-2015
Leif Svalgaard

TL;DR
This paper reconstructs the historical solar EUV flux from geomagnetic data spanning over 275 years, revealing its correlation with solar activity indicators and suggesting a consistent minimum flux level during solar minima.
Contribution
It introduces a method to reliably reconstruct solar EUV flux from geomagnetic records dating back to the 1830s, extending understanding of solar magnetic activity over centuries.
Findings
Reconstructed EUV flux matches F10.7 flux accurately.
EUV flux reaches a consistent low during minima, indicating an invariant solar magnetic ground state.
Current sunspot number may not fully represent solar magnetic activity.
Abstract
Solar Extreme Ultraviolet (EUV) radiation creates the conducting E-layer of the ionosphere, mainly by photo ionization of molecular Oxygen. Solar heating of the ionosphere creates thermal winds which by dynamo action induce an electric field driving an electric current having a magnetic effect observable on the ground, as was discovered by G. Graham in 1722. The current rises and sets with the Sun and thus causes a readily observable diurnal variation of the geomagnetic field, allowing us the deduce the conductivity and thus the EUV flux as far back as reliable magnetic data reach. High-quality data go back to the 'Magnetic Crusade' of the 1830s and less reliable, but still usable, data are available for portions of the hundred years before that. J.R. Wolf and, independently, J.-A. Gautier discovered the dependence of the diurnal variation on solar activity, and today we understand and…
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