Published December 5, 2022
| Version v1
Report
Open
Radiofrequency Ice Dielectric Measurements at Summit Station, Greenland
Creators
- Aguilar, J. A.1
- Allison, P.2
- Besson, D.3
- Bishop, A.4
- Botner, O.5
- Bouma, S.6
- Buitink, S.7
- Cataldo, M.6
- Clark, B. A.8
- Couberly, K.3
- Curtis-Ginsberg, Z.9
- Dasgupta, P.1
- de Kockere, S.7
- de Vries, K. D.7
- Deaconu, C.9
- DuVernois, M. A.4
- Eimer, A.6
- Glaser, C.5
- Hallgren, A.5
- Hallmann, S.10
- Hughes, K.9
- Michaels, K.9
- Oberla, E.9
- Smith, D.9
- Southall, D.9
- Vieregg, A. G.9
- Welling, C.9
- 1. Université Libre de Bruxelles
- 2. The Ohio State University
- 3. University of Kansas
- 4. University of Wisconsin-Madison
- 5. Uppsala University
- 6. Friedrich-Alexander-University Erlangen-Nürnberg
- 7. Vrije Universiteit Brussel
- 8. Michigan State University
- 9. University of Chicago
- 10. Deutsches Elektronen-Synchrotron DESY
Description
We recently reported (Aguilar and others, 2022) on the radio-frequency attenuation length of cold polar ice at Summit Station, Greenland, based on bistatic radar measurements of radio frequency bedrock echo strengths taken during the summer of 2021. Those data also include echoes attributed to stratified impurities or dielectric discontinuities within the ice sheet ("layers"), which allow studies of a) estimation of the relative contribution of coherent (discrete layers, e.g.) vs. incoherent (bulk volumetric, e.g.) scattering, b) the magnitude of internal layer reflection coefficients, c) limits on the azimuthal asymmetry of reflections ('birefringence'), and d) limits on signal dispersion in-ice over a bandwidth of ~100 MHz. We find that i) after averaging 10000 echo triggers, reflected signal observable over the thermal floor (to depths of approximately 1500 m) are consistent with being entirely coherent, ii) internal layer reflection coefficients are measured at approximately –60 to –70 dB, iii) birefringent effects for vertically propagating signals are smaller by an order of magnitude relative to comparable studies performed at South Pole, and iv) within our experimental limits, glacial ice is non-dispersive over the frequency band relevant for neutrino detection experiments.
Files
Radio_frequency_echo_measurements_at_Summit_Station__Greenland.pdf
Files
(2.3 MB)
| Name | Size | Download all |
|---|---|---|
|
md5:6375bbbde309ac0a3992746169e596de
|
2.3 MB | Preview Download |
Additional details
Identifiers
- Other
- oai:uchicago.tind.io:5158
Funding
- Belgian Funds for Scientific Research
- FWO Programme for International Research Infrastructure
- National Science Foundation
- 2118315
- National Science Foundation
- 2112352
- IceCube EPSCoR Initiative
- 2019597
- German Research Foundation
- NE 2031/2-1
- Helmholtz Association
- Initiative and Networking Fund
- European Research Council
- 805486