REVIEW 3 major objections 5 minor 19 references
First measurements with prototype radio antennas for the IceTop detector array
T0 review · 3 major / 5 minor · reviewed 2026-08-14 · deepseek-v4-flash
Pith's one-line read South Pole radio antennas pick up unexplained peaks every 10 MHz
desk verdict A useful, honest engineering status report; the deployment and LNA work are solid, but the RFI/background excess rests on an uncalibrated absolute baseline and should be read with skepticism. read the letter →
The pith
A machine-rendered reading of the paper's core claim, the machinery that carries it, and where it could break.
The reading
What carries the argument
The central object is the SKALA-2 prototype antenna, a wideband antenna covering roughly 70 to 350 MHz with a low-noise amplifier whose gain stays constant within about 2 dB from 20 °C down to -70 °C. It is paired with the hybrid TAXI data-acquisition system, a DRS4-based readout platform that digitizes scintillator and radio signals at 1 GHz, preceded by a radio front-end board that filters the signal to about 50 to 350 MHz. The comparison baseline is the expected amplified sky background, built from the sky-noise model, the simulated amplifier gain, and a fixed 30 K thermal-noise contribution; this predicted curve is the reference that makes the measured field spectra look higher than expected.
What would settle it
Replace the simulated amplifier gain in the expected spectrum with the low-noise-amplifier gain actually measured at low temperature (shown in the paper's Fig. 2) and recompute the comparison; if the excess over the sky-noise prediction disappears or the 10 MHz peaks no longer sit above the recalibrated baseline, the paper's central interpretation is not supported.
Extended reading notes
Core claim
On the paper's own terms, the SKALA prototype antenna with its internal low-noise amplifier and the TAXI-based hybrid DAQ that digitizes both scintillator and radio signals operated successfully at the South Pole. In two one-hour background measurements taken about 25 meters from the central laboratory building, the measured spectra exceed the expected amplified sky background computed from the sky-noise model together with a simulated amplifier gain and a 30 K thermal-noise contribution. Both spectra show RFI peaks that become visible at 50 MHz and reappear every 10 MHz; the source is unknown, with nearby electronics inside the laboratory a plausible origin. The antenna polarization aimed toward the laboratory records more noise than the perpendicular polarization, as expected from a nearby noise source.
Load-bearing premise
The load-bearing premise is that the simulated low-noise-amplifier gain, the 30 K thermal-noise contribution, and the sky-noise model together give an accurate absolute calibration, because every claim of an unexpected excess or periodic peaks is read against that predicted curve.
Editorial extensions
If this is right
- The prototype station's mechanics and electronics can survive South Pole conditions, so the deployment method can be scaled to the planned 32-station, 96-antenna array.
- The hybrid DAQ successfully samples particle and radio signals together, demonstrating the technical basis for a combined surface detector that records both air-shower components.
- The radio environment within about 25 meters of the central laboratory building carries periodic interference at 10 MHz intervals, so any physics array must either move away from such infrastructure, shield it, or identify and remove the source.
- If the excess over the sky-noise prediction is real, the absolute calibration of the full array will need to include additional thermal or local noise contributions beyond the model.
Reading between the lines
- My inference: the strict 10 MHz spacing of the RFI peaks points to a digital clock or switching power supply near the antennas; because the high-pass filter starts near 50 MHz, a single 50 MHz or 100 MHz harmonic source could produce the observed comb.
- My inference: the comparison against an absolute sky-noise curve rests on the simulated amplifier gain, so redoing the prediction with the measured gain from the paper's own Fig. 2 would show how much of the reported excess is calibration-dependent.
- My inference: repeating the same background measurement with the antenna moved kilometers away from the central laboratory, at the position of the permanent prototype array, would determine whether the excess and peaks are local infrastructure or a genuinely unexpected South Pole background.
- My inference: if the 10 MHz comb extends across the 50 to 350 MHz band, it could also mask the radio air-shower pulses the array is designed to detect, so a time-domain check of whether the interference is continuous or intermittent would be a cheap next step.
Signed reviews
Editorial analysis
A structured set of objections, weighed in public.
Referee Report
Summary. This ICRC2019 proceeding reports the deployment, in January 2019 at the South Pole, of two prototype SKALA radio antennas for a future hybrid IceTop extension, together with a TAXI-based DAQ system that reads out both scintillation detectors and radio antennas. The paper describes the mechanical design and deployment, presents a laboratory characterization of the LNA gain as a function of temperature (20 C to -70 C), and gives first background spectra measured about 25 m from the IceCube Laboratory (ICL). The authors state that the measured spectra show RFI-like peaks recurring every 10 MHz starting near 50 MHz and that the overall level is higher than an expected sky-noise prediction based on the Cane model and an antenna/LNA simulation. The conclusion is explicitly preliminary: the origin of the RFI and of the discrepancy with the prediction is said to be unclear, and further measurements with the deployed antennas are planned.
Significance. If the reported behavior is taken at face value, the paper demonstrates that the SKALA mechanical structure and the hybrid TAXI DAQ can be operated at the South Pole, and it provides an early indication that the radio background near existing South Pole infrastructure is not purely sky-noise limited. The careful LNA temperature characterization is a useful engineering contribution. The strength of the environmental conclusion, however, is limited by the absence of an end-to-end absolute calibration and the lack of statistical error bars on the spectra; these are acknowledged as open items in the text but currently prevent the quantitative 'higher than expected' and 'RFI' claims from being fully supported. The paper is appropriately modest in tone and is best read as a progress report rather than as a definitive measurement of the South Pole radio environment.
major comments (3)
- [Section 5, Fig. 6] The absolute baseline used to conclude that the measured spectra are 'higher than the expectation of the sky noise' is assembled from the simulated LNA gain of de Lera Acedo et al. [17], a constant 30 K thermal-noise contribution, and the Cane sky model, rather than from the LNA gain actually measured in Section 2, Fig. 2. Since the measured LNA gain is available, using the simulated gain introduces an avoidable and unquantified calibration uncertainty; a frequency-dependent difference between the simulated and the deployed LNA gain would translate directly into an apparent spectral excess or deficit. I request that the comparison use the measured gain (with any necessary corrections for the cable and filter chain) and that the expected absolute level be propagated with explicit uncertainties.
- [Section 5, Fig. 6] The two one-hour average spectra are shown without any error bars, confidence bands, or estimate of systematic uncertainties, so the visual 'excess' over the black dashed prediction cannot currently be distinguished from statistical noise or from systematic baseline effects. In addition, the claimed 10 MHz periodicity of the peaks is a spectral ripple pattern that can be produced by impedance mismatches and reflections in the 30 m cable and front-end chain; without a system-noise-only measurement, a calibration-source measurement through the same signal path, or a cable-length scan, the identification of these features as ambient RFI is premature. The paper's own statement that the origin of the discrepancy is unclear reinforces this point, but the current wording of the results and conclusion still presents the peaks and the excess as established measurements.
- [Section 5, paragraph 3] The description of the expected background is incomplete for reproducibility: the paper does not state the absolute units of Fig. 6, the assumed antenna elevation/azimuth response, the cable attenuation as a function of frequency, or how the 'amplified sky radio background' combines the Cane-model sky temperature with the individual gain and loss terms. Without these definitions, the quantitative comparison in Fig. 6 cannot be independently checked, and the statement that 'a slight deviation of the expectation and the measurement is expected' is not sufficient to interpret the size of the observed discrepancy.
minor comments (5)
- [Section 5, Fig. 6 caption] The caption should specify the y-axis units and the exact frequency binning used for the average spectra, as well as whether the solid and dashed black lines correspond to the sky temperature before and after amplification, respectively.
- [Section 6, last sentence] The phrase 'radio antennas wthat share one DAQ system' contains a typo; it should read 'that share one DAQ system'.
- [Section 2, Fig. 2] The caption states that the LNA gain was measured with a 50-ohm calibration source, but the text does not give the absolute power level or the number of repeated measurements used to quote the 'about 2 dB' temperature stability; adding this information would strengthen the reproducibility of the test.
- [Section 3] The sentence 'The trigger is realized with a comparator as a signal-over-threshold trigger' would be clearer if it distinguished the comparator threshold for the scintillator channels from the threshold used for the radio channels, since the current text says that the trigger is based only on scintillation detectors.
- [Section 1] The abbreviation 'GFK' (glass-fiber reinforced plastic) is used without expansion; I suggest using the more common GFRP or defining GFK at first use.
Circularity Check
No circularity: the measured spectra and external-model comparisons are not derived from the paper's own inputs.
full rationale
All scientific claims in the paper are either direct hardware/DAQ reports or empirical spectral measurements. The expectation line in Fig. 6 is built from external, published inputs: the Cane sky model [18], the simulated LNA gain from de Lera Acedo et al. [17], a constant 30 K thermal-noise contribution, and known filter/cable losses; none of these are fitted to the measured spectra shown in Fig. 6, and no target quantity is defined in terms of the measurement. The paper explicitly flags the calibration limitations: 'As LNA response, the simulated LNA gain from E. de Lera Acedo et al. [17] has been used' and 'The deviation could come from an additional thermal noise contribution which has not been included in the amplified background estimation' (Section 5). This is an unvalidated absolute calibration pointing to a correctness or systematic-uncertainty concern, not circularity. The 10 MHz periodic RFI peaks are read directly from the averaged measured spectra, not generated by inverting a model or by a fitted parameter. No load-bearing self-citation occurs: [17] is an external antenna/LNA design simulation, [18] is the standard Cane sky-noise model, and [13] is the TAXI DAQ reference; none of these is used to import a uniqueness theorem or to forbid alternative interpretations. Therefore no fitted input is relabeled as a prediction, and no equation reduces to the paper's own inputs.
Assumptions & free parameters
assumptions (3)
- domain assumption The simulated SKALA LNA response from [17] accurately represents the deployed LNA at South Pole temperatures.
- domain assumption The Cane model provides a valid sky-noise prediction for the South Pole.
- domain assumption The observed 10 MHz-spaced RFI peaks are environmental rather than artifacts of the DAQ or front-end chain.
Cite this review
Pith. "Pith review of First measurements with prototype radio antennas for the IceTop detector array." pith.science (2026). https://pith.science/paper/4NEU6DUX
@misc{pith2026190810565,
author = {Pith},
title = {Pith review of: First measurements with prototype radio antennas for the IceTop detector array},
year = {2026},
howpublished = {\url{https://pith.science/paper/4NEU6DUX}},
note = {Machine review of arXiv:1908.10565}
}
abstract
Extending large-scale air-shower arrays with radio antennas can increase the detector's performance, as the radio emission by cosmic-ray air showers provides an additional measurement of the electromagnetic component. Instrumenting the IceCube surface detector IceTop with radio detectors as well as with new particle detectors in a hybrid approach will enhance the measurement and reconstruction accuracy and allow for the characterization of highly inclined air showers. This will enable a better understanding of the atmospheric background for the in-ice neutrino measurements. It also opens the opportunity for new science cases, e.g. the search for PeV gamma rays from the Galactic Center, which is visible from the IceCube site year-round at an inclination of 61$^{\circ}$. Adding to several scintillator particle detectors already running at the South Pole, two prototype radio antennas have been deployed at the IceCube site in January 2019 using the same DAQ system as the scintillators. The antennas serve as a test setup for a future deployment of radio antennas extending the scintillator array planned inside the IceTop footprint. In this proceeding, the antennas considered for deployment and the hybrid DAQ system processing the signals of the particle and radio detectors will be introduced. First measurement results at the South Pole will be presented and future plans for a full hybrid particle and radio detector array inside the IceTop footprint will be shown.
Figures
Figures from the paper (3 more)
Reference graph
Works this paper leans on
-
[17]
E. de Lera Acedo, N. Drought, B. Wakley, and A. Faulkner, 2015 International Conference on Electromagnetics in Advanced Applications (ICEAA) (Sep., 2015) 839–843
work page 2015
-
[1]
IceCube Collaboration, M. G. Aartsen et al., JINST 12 (2017) P03012
2017
-
[2]
IceCube Collaboration, M. G. Aartsen et al., arXiv:1412.5106
-
[3]
Kunwar, T
IceCube-Gen2 Collaboration, S. Kunwar, T. Huber, J. Kelley, and D. Tosi,PoS(ICRC2017)401 (2018)
2018
-
[4]
Auffenberg, PoS(ICRC2017)1055 (2018)
IceCube Gen2 Collaboration, J. Auffenberg, PoS(ICRC2017)1055 (2018)
2018
-
[5]
F. G. Schröder, EPJ Web Conf. 208 (2019) 15001
work page 2019
-
[6]
F. G. Schröder, Prog. Part. Nucl. Phys. 93 (2017) 1–68
2017
-
[7]
Huege, Phys
T. Huege, Phys. Rept. 620 (2016) 1–52
2016
Show all 19 references
-
[8]
Tunka-Rex, LOPES Collaboration, W. D. Apel et al., Phys. Lett. B763 (2016) 179–185
2016
-
[9]
HESS Collaboration, Nature 531 (2016) 476 – 479
2016
-
[10]
Balagopal V ., A
A. Balagopal V ., A. Haungs, T. Huege, and F. G. Schröder,Eur . Phys. J.C78 (2018) 111
2018
-
[11]
IceCube Collaboration, F. G. Schröder, PoS(ICRC2019)418,these proceedings (2019)
2019
-
[12]
de Lera Acedo, N
E. de Lera Acedo, N. Razavi-Ghods, N. Troop, N. Drought, and A. J. Faulkner, Experimental Astronomy 39 (Oct, 2015) 567–594
2015
-
[13]
T. Karg, A. Haungs, M. Kleifges, R. Nahnhauer, and K. H. Sulanke, 6th International Workshop on Acoustic and Radio EeV Neutrino Detection Activities (ARENA 2014) Annapolis, MD, June 9-12, 2014 (2014)
2014
-
[14]
Allison, J
ARA Collaboration, P. Allison, J. Auffenberg, R. Bard, J. J. Beatty, D. Z. Besson, S. Böser, C. Chen, P. Chen, and A. Connolly, Astroparticle Physics 35 (Feb, 2012) 457–477
2012
-
[15]
Böser, AIP Conference Proceedings 1535 (2013) 116–120
ARA, IceCube Collaborations, S. Böser, AIP Conference Proceedings 1535 (2013) 116–120
2013
-
[16]
Auffenberg, T
J. Auffenberg, T. Gaisser, K. Helbing, T. Huege, T. Karg, and A. Karle, Nucl. Instrum. Meth. A604 (2009) S53–S56
2009
-
[18]
H. V . Cane, Monthly Notices of the Royal Astronomical Society 189 (Nov., 1979) 465–478
1979
-
[19]
Kauer, PoS(ICRC2019)309,these proceedings (2019)
IceCube Collaboration, M. Kauer, PoS(ICRC2019)309,these proceedings (2019). 8
2019
Reviewed August 14, 2026 · model on record in the stance chip above.
Discussion (0). Continue with ORCID to comment.