Earth as a transducer for dark-photon dark-matter detection
Michael A. Fedderke, Peter W. Graham, Derek F. Jackson Kimball, and, Saarik Kalia

TL;DR
This paper proposes using the Earth as a natural detector for ultralight dark-photon dark matter by identifying a global magnetic field signal at Earth's surface, enabling new detection strategies for this elusive particle.
Contribution
The paper introduces a novel method of dark-photon detection leveraging Earth's surface magnetic field pattern, extending sensitivity to lower masses than laboratory experiments.
Findings
No robust signal candidates found in SuperMAG data
Constraints placed on dark-photon mass range from $2\times 10^{-18}$ to $7\times 10^{-17}$ eV
Method demonstrates potential for future ultralight dark-matter searches
Abstract
We propose the use of the Earth as a transducer for ultralight dark-matter detection. In particular we point out a novel signal of kinetically mixed dark-photon dark matter: a monochromatic oscillating magnetic field generated at the surface of the Earth. Similar to the signal in a laboratory experiment in a shielded box (or cavity), this signal arises because the lower atmosphere is a low-conductivity air gap sandwiched between the highly conductive interior of the Earth below and ionosphere or interplanetary medium above. At low masses (frequencies) the signal in a laboratory detector is usually suppressed by the size of the detector multiplied by the dark-matter mass. Crucially, in our case the suppression is by the radius of the Earth, and not by the (much smaller) height of the atmosphere. We compute the size and global vectorial pattern of our magnetic field signal, which enables…
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