4.5 Article

Dark Matter Detection in the Stratosphere

期刊

SYMMETRY-BASEL
卷 15, 期 6, 页码 -

出版社

MDPI
DOI: 10.3390/sym15061167

关键词

streaming dark matter; direct detection; stratospheric anomaly

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We investigate the prospects for directly detecting dark matter particles in the upper atmosphere. A recent study suggests a relationship between burst-like temperature fluctuations in the stratosphere at heights of 38-47 km and low-speed invisible streaming matter, which motivates this proposal. Dark photons, emerging as a U(1) symmetry within extensions of the standard model, could provide an explanation if they are part of the local dark matter density. In addition, the ionospheric plasma column above the stratosphere can enhance the conversion of dark photons to photons via resonance, and the stratosphere is easily accessible for balloon flights.
We investigate the prospects for the direct detection of dark matter (DM) particles, incident on the upper atmosphere. A recent work relating the burst-like temperature excursions in the stratosphere at heights of & AP;38-47 km with low speed incident invisible streaming matter is the motivation behind this proposal. As an example, dark photons could match the reasoning presented in that work provided they constitute part of the local DM density. Dark photons emerge as a U(1) symmetry within extensions of the standard model. Dark photons mix with real photons with the same total energy without the need for an external field, as would be required, for instance, for axions. Furthermore, the ionospheric plasma column above the stratosphere can resonantly enhance the dark photon-to-photon conversion. Noticeably, the stratosphere is easily accessible with balloon flights. Balloon missions with up to a few tons of payload can be readily assembled to operate for months at such atmospheric heights. This proposal is not limited to streaming dark photons, as other DM constituents could be involved in the observed seasonal heating of the upper stratosphere. Therefore, we advocate a combination of different types of measurements within a multi-purpose parallel detector system, in order to increase the direct detection potential for invisible streaming constituents that affect, annually and around January, the upper stratosphere.

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