Part 3

Reconstructing the Sky

Detecting a neutrino is not astronomy. Astronomy needs a direction, and ideally an energy. IceCube gets them from two different kinds of event, and the frustrating part โ€” the thing that shapes every analysis the collaboration does โ€” is that no single event gives you both well.

Why a muon is the best messenger

A muon loses energy in two ways. At low energy it ionises atoms at a roughly constant rate; at high energy it radiates โ€” bremsstrahlung, pair production, photonuclear losses โ€” at a rate proportional to its energy. Together:

\[ -\frac{dE}{dx} = a + bE \]

with a โ‰ˆ 0.26 GeV/m and b โ‰ˆ 3.6 ร— 10โปโด mโปยน in ice (approximate values). Separating and integrating from E down to zero gives the range:

\[ R = \int_0^{E}\frac{dE'}{a + bE'} = \frac{1}{b}\ln\!\left(1 + \frac{bE}{a}\right) \]

The logarithm is the whole story. Energy buys range, but only logarithmically:

Muon energyRange in ice
100 GeV0.36 km
1 TeV2.4 km
100 TeV13.7 km
1 PeV20.1 km

A 100 TeV muon travels fourteen kilometres through ice โ€” fourteen times the width of the detector. This is the quiet reason IceCube works far better than its instrumented volume suggests: a neutrino can interact a long way outside the array and still send a muon through it. The detector's effective volume for muon events is much larger than the cubic kilometre Part 2 paid for.

Muon range in ice rising logarithmically with energy, crossing the one-kilometre detector scale well below a TeV.
Figure 5. Range against energy. Above about 500 GeV the muon outruns the detector, so the track enters and leaves โ€” which fixes the direction beautifully and ruins the energy measurement.

Two event shapes, two trade-offs

Which shape you get depends on the interaction the primer described, and on the flavour of the neutrino that arrived.

Two schematic event displays: an elongated track crossing the array, and a compact spherical cascade.
Figure 6. A track crosses the array; a cascade sits inside it.

Tracks

A muon neutrino interacts by charged current and makes a muon, which crosses the detector in a straight line. Timing the Cherenkov light along a kilometre-long lever arm fixes the direction to roughly half a degree.

But the muon was made outside and leaves still carrying energy, so the deposited light is only a lower bound on the neutrino's energy.

Cascades

A neutral-current interaction, or an electron neutrino, dumps its energy into a shower only a few metres long โ€” effectively a point source of light inside the array. Contained, so nearly all the energy is measured: roughly 15% accuracy.

But a glowing sphere has almost no directional information. Angular resolution is ten to fifteen degrees โ€” a patch of sky containing many candidate sources.

What actually limits the pointing

Naively the angular resolution should follow from timing alone. With sensors timed to a few nanoseconds and a lever arm L of a kilometre, the angular error is roughly

\[ \Delta\theta \sim \frac{c\,\Delta t}{n\,L} \]

which for ฮ”t = 3 ns gives under a tenth of a degree. The real figure is several times worse, and the reason is the ice itself: photons scatter many times on their way to a sensor, so the arrival time carries a long random tail. The limit is not the clock, it is the medium.

This is why mapping the optical properties of the ice โ€” layer by layer, through dust bands laid down over a hundred thousand years โ€” turned out to be as much a part of the experiment as the electronics. The detector had to learn the glacier it was frozen into.

Check your understanding

  1. Why does a search for a point source use tracks, while a measurement of the diffuse spectrum prefers cascades?
    Answer: a point source needs direction, which only tracks supply; a spectrum needs energy, which only contained cascades supply.
  2. At what energy does the muon range first exceed the detector size, and what changes there?
    Answer: around 500 GeV. Above it the muon no longer stops inside, so events become through-going: direction improves, contained energy is lost.
  3. If you could halve the sensor timing jitter, would the pointing improve by a factor of two?
    Answer: no. Photon scattering in the ice dominates, so the clock is not the binding constraint.

What this leaves out

The energy-loss coefficients a and b themselves depend weakly on energy, and radiative losses are stochastic rather than smooth โ€” a muon can lose a large fraction of its energy in a single burst, which both brightens the track and spoils the simple picture of steady decline. Resolution figures quoted here are representative rather than exact; they depend on energy and on the reconstruction used.

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