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Cosmic Rays and the Sky

More cosmic-ray muons reach the ground the higher you go, and Nepal's climb from the plains to the high Himalaya is the place to measure it: muon detectors along the transect, and for meteors, the all-sky camera and then radar.
Planned

How the particles from space change with height

Cosmic rays strike the top of the atmosphere and make showers of particles. The ones that reach the ground are mostly muons, and there are more of them the higher you go, because there is less air overhead to stop them. Nepal climbs nearly 8,800 m in under 200 km, which makes it the place to measure how the muon rate changes along the climb.

A muon lives about 2.2 microseconds. Even at nearly the speed of light that is too short to cross 15 km of air, yet muons arrive in large numbers: their clocks run slow, which is relativistic time dilation.

Cosmic-Ray Muons

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A muon made about 15 km up should decay long before it reaches the ground. Play it through: time dilation is why it does not, and why a detector at 4,000 m counts more than one at 100 m.

How much air is overhead, the atmospheric depth, falls off roughly exponentially with height, and the muon rate follows it:

Atmospheric depth against altitude. X₀ ≈ 1,033 g/cm² at sea level; the scale height H ≈ 8.5 km.
Muon rate against altitude, expected

A model: the curve these measurements are meant to test. Marked points are planned sites.

Air pressure at the planned sites today

Lower pressure means less air overhead and more muons. These pressures are weather-model estimates for each site.

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Source: Open-Meteo weather forecast models · CC BY 4.0.
Source: Open-Meteo air quality, from the Copernicus Atmosphere Monitoring Service (CAMS) · CC BY 4.0; contains modified Copernicus Atmosphere Monitoring Service information.
Borders: Natural Earth, public domain.

An open design, adapted for the Himalaya

The detector will be based on CosmicWatch, an open design from MIT: a plastic scintillator, a silicon photomultiplier and a small microcontroller, which we are adapting for Himalayan deployment: cold, damp and long runs on solar power. Two units stacked in coincidence count only the particles that pass through both, which rejects most of the background. Each count is logged with the air pressure, so readings at different heights can be compared. The plan is a pair beside each IESH hub along the transect, from Nepalgunj at about 150 m to Dho Tarap at about 4,000 m.

→ The muon detector

The all-sky camera, then radar

The full IESH station is designed to carry an all-sky camera, which would record meteors as well as cloud. Radar comes after it: a meteor's trail of ionised air reflects radio waves, so radar sees meteors by day and through cloud. HICS's founder has published work using meteor-radar data (Physical Review D, 2023).

Radar Meteor Detection

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What a radar echo from a meteor trail looks like.
Current status

Planned. The muon detector will be based on CosmicWatch, adapted for Himalayan deployment, with one beside each IESH hub on the transect. The all-sky camera is part of the full IESH station design.

2023
Physical Review D
New Constraints on Macroscopic Dark Matter Using Radar Meteor Detectors
Pawan Dhakal, Steven Prohira, Christopher V. Cappiello, John F. Beacom, Scott Palo, John Marino
doi:10.1103/PhysRevD.107.043026